鲁西地区龙宝山碱性杂岩体岩石成因与稀土元素富集机制

doi:10.13745/j.esf.sf.2025.1.31

地学前缘 ›› 2026, Vol. 33 ›› Issue (2): 265-289.DOI: 10.13745/j.esf.sf.2025.1.31

• 战略矿产成因机制与金属富集 • 上一篇下一篇

鲁西地区龙宝山碱性杂岩体岩石成因与稀土元素富集机制

刘传朋¹^,²(), 马钊¹^,²^,^*(), 安茂国²^,³^,^*(), 支成龙¹^,², 杨泽宇⁴, 吴鸣谦⁴^,⁵, 尚振¹^,², 陈怀鑫¹^,², 韩宗瑞¹^,², 姜腾飞¹^,², 高文白¹^,²

1.山东鲁南地质工程勘察院(山东省地质矿产勘查开发局第二地质大队), 山东济宁 272100
2.三稀矿产勘查与综合利用山东省工程研究中心, 山东济宁 272100
3.山东省第三地质矿产勘查院, 山东烟台 264004
4.中国地质大学(北京) 地质过程与成矿预测国家重点实验室, 地球科学与资源学院, 北京 100083
5.温莎大学环境学院, 加拿大温莎 N9B 3P 4

收稿日期:2025-04-11 修回日期:2025-08-05 出版日期:2026-03-25 发布日期:2026-01-29
通信作者: *马钊(1997—),男,硕士,助理工程师,主要从事岩石地球化学及地质勘查等工作。E-mail: mazxxx@foxmail.com; 安茂国(1984—),男,硕士,正高级工程师,主要从事区域地质调查及矿产勘查等工作。E-mail: 15963775283@163.com
作者简介:刘传朋(1981—),男,硕士,正高级工程师,主要从事区域地质调查及矿产勘查等工作。E-mail: liuchuanpeng666@163.com
基金资助:
山东省鲁南地质工程勘察院(山东省地质矿产勘查开发局第二地质大队)及三稀矿产勘查与综合利用山东省工程研究中心开放基金项目(LNY202206);山东省鲁南地质工程勘察院(山东省地质矿产勘查开发局第二地质大队)及三稀矿产勘查与综合利用山东省工程研究中心开放基金项目(LNY202301);山东省鲁南地质工程勘察院(山东省地质矿产勘查开发局第二地质大队)及三稀矿产勘查与综合利用山东省工程研究中心开放基金项目(LNY202302)

Petrogenesis and rare earth element enrichment of the Longbaoshan alkaline complex, Luxi region

LIU Chuanpeng¹^,²(), MA Zhao¹^,²^,^*(), AN Maoguo²^,³^,^*(), ZHI Chenglong¹^,², YANG Zeyu⁴, WU Mingqian⁴^,⁵, SHANG Zhen¹^,², CHEN Huaixin¹^,², HAN Zongrui¹^,², JIANG Tengfei¹^,², GAO Wenbai¹^,²

1. Shandong Provincial Lunan Geology and Exploration Institute (Shandong Provincial Bureau of Geology and Mineral Resources No.2 Geological Brigade), Jining 272100, China
2. Rare Mineral Exploration and Comprehensive Utilization Engineering Research Center of Shandong Province, Jining 272100, China
3. Shandong Provincial No.3 Exploration Institute of Geology and Mineral Resources, Yantai 264004, China
4. State key Laboratory of Geological Processes and Mineral Resources/School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, China
5. School of the Environment, University of Windsor, Windsor N9B 3P4, Canada

Received:2025-04-11 Revised:2025-08-05 Online:2026-03-25 Published:2026-01-29

摘要/Abstract

摘要：

龙宝山碱性杂岩体位于华北克拉通鲁西地区东南缘,是新发现的龙宝山稀土矿的赋矿岩体,但其岩石成因和稀土富集机制仍没有得到很好的解释。本文对该碱性杂岩体中的正长斑岩、石英正长斑岩、含角闪正长斑岩的岩石地球化学特征进行了系统的研究,旨在限定该岩体的成因机制,揭示稀土元素的富集机制。研究结果显示,龙宝山碱性杂岩体形成于早白垩世(130~128 Ma),所分析样品具有较高的SiO₂、Na₂O、K₂O和Al₂O₃含量以及较低的MgO、FeO和CaO含量,属于准铝质岩、过碱性岩、高钾钙碱性岩和钾玄岩。样品都表现出富集的Sr-Nd同位素特征,富集大离子亲石元素(large-ion lithophile element,LILE)和轻稀土元素(light rare earth element,LREE),亏损Nb、Ta和Ti重稀土元素(heavy rare earth element,HREE),且具较高的Nb/Y、Th/Yb、La/Sm和较低的Ba/Th值,这些均指示俯冲沉积物熔体交代了地幔源区并为源区提供了稀土元素的初始富集。在岩浆演化早期,角闪石和黑云母的分离结晶促进了稀土元素的进一步富集。钠长石交代是热液作用的结果,岩浆晚期的热液交代作用导致了稀土元素的富集成矿。因此,龙宝山碱性杂岩体起源于富集岩石圈地幔的部分熔融,俯冲海洋沉积物再循环诱发的稀土元素(rare earth elements,REE)初始富集对龙宝山碱性岩型稀土矿床的形成具有重要制约,岩浆-热液作用过程是稀土元素富集成矿的关键过程。

关键词: 龙宝山碱性杂岩体, 稀土富集机制, 地幔交代作用, 华北克拉通

Abstract:

The Longbaoshan alkaline complex, located in the southeastern Luxi Terrane of the North China Craton, hosts a newly discovered REE deposit. However, the petrogenesis of the complex and the mechanisms of rare earth element (REE) enrichment remain poorly understood. This study presents a systematic investigation of the whole-rock geochemistry of the syenite porphyry, quartz syenite porphyry, and amphibole-bearing syenite porphyry within the complex, aiming to elucidate its petrogenesis and reveal the REE enrichment mechanisms. The results indicate that the Longbaoshan alkaline complex formed in the Early Cretaceous (130-128 Ma). It is characterized by high SiO₂, Na₂O + K₂O, and Al₂O₃ contents, but low MgO, FeO, and CaO, displaying metaluminous to peralkaline and belongs to the high-K calc-alkaline to shoshonitic series. All samples exhibit enriched Sr-Nd isotopic compositions and are enriched in large-ion lithophile element (LILE) and light rare earth element (LREE), but are depleted in high field strength element (HFSE; e.g., Nb, Ta, Ti) and heavy rare earth element (HREE). They also feature low Ba/Th and high Nb/Y, Th/Yb, and La/Sm ratios. These geochemical characteristics suggest that the mantle source was metasomatized by melts derived from subducted sediments, which provided the initial REE enrichment. During early magmatic evolution, fractional crystallization of hornblende and biotite promoted further enrichment of REE. The albitization results from hydrothermal processes, and late magmatic-hydrothermal metasomatism resulted in ore-forming REE enrichment. Therefore, the Longbaoshan alkaline complex originated from the partial melting of enriched lithospheric mantle. Initial REE enrichment by metasomatic subduction-related melts was crucial for mineralization, while subsequent magmatic-hydrothermal processes were key to further enrichment and ore formation.

Key words: Longbaoshan alkaline complex, REE enrichment, mantle metasomatism, the North China Craton

中图分类号:

刘传朋, 马钊, 安茂国, 支成龙, 杨泽宇, 吴鸣谦, 尚振, 陈怀鑫, 韩宗瑞, 姜腾飞, 高文白. 鲁西地区龙宝山碱性杂岩体岩石成因与稀土元素富集机制[J]. 地学前缘, 2026, 33(2): 265-289.

LIU Chuanpeng, MA Zhao, AN Maoguo, ZHI Chenglong, YANG Zeyu, WU Mingqian, SHANG Zhen, CHEN Huaixin, HAN Zongrui, JIANG Tengfei, GAO Wenbai. Petrogenesis and rare earth element enrichment of the Longbaoshan alkaline complex, Luxi region[J]. Earth Science Frontiers, 2026, 33(2): 265-289.

图/表 20

参考文献 118

[1]	付瑞鑫, 李宁波, 牛贺才, 等. 赛马碱性杂岩体的岩浆演化与稀土富集[J]. 岩石学报, 2023, 39(10): 2951-2967.
[2]	BONIN B, AZZOUNI-SEKKAL A, BUSSY F, et al. Alkali-calcic and alkaline post-orogenic (PO) granite magmatism: petrologic constraints and geodynamic settings[J]. Lithos, 1998, 45(1/2/3/4): 45-70. DOI URL
[3]	LIÉGEOIS J P, NAVEZ J, HERTOGEN J, et al. Contrasting origin of post-collisional high-K calc-alkaline and shoshonitic versus alkaline and peralkaline granitoids. The use of sliding normalization[J]. Lithos, 1998, 45(1/2/3/4): 1-28. DOI URL
[4]	UPADHYAY D, RAITH M M, MEZGER K, et al. Mesoproterozoic rift-related alkaline magmatism at Elchuru, Prakasam Alkaline Province, SE India[J]. Lithos, 2006, 89(3/4): 447-477. DOI URL
[5]	JUNG S, HOFFER E, HOERNES S. Neo-Proterozoic rift-related syenites (Northern Damara Belt, Namibia): geochemical and Nd-Sr-Pb-O isotope constraints for mantle sources and petrogenesis[J]. Lithos, 2007, 96(3/4): 415-435. DOI URL
[6]	SHELLNUTT J G, ZHOU M-F. Permian, rifting related fayalite syenite in the Panxi region, SW China[J]. Lithos, 2008, 101(1/2): 54-73. DOI URL
[7]	ASHWAL L, TORSVIK T, HORVÁTH P, et al. A mantle-derived origin for Mauritian trachytes[J]. Journal of Petrology, 2016, 57(9): 1645-1676.
[8]	LAPORTE D, LAMBART S, SCHIANO P, et al. Experimental derivation of nepheline syenite and phonolite liquids by partial melting of upper mantle peridotites[J]. Earth and Planetary Science Letters, 2014, 404: 319-331. DOI URL
[9]	EBY G. Geochemistry and petrogenesis of nepheline syenites: Kasungu-Chipala, Ilomba, and Ulindi nepheline syenite intrusions, North Nyasa alkaline province, Malawi[J]. Journal of Petrology, 1998, 39(8): 1405-1424. DOI URL
[10]	IRVING A J, PRICE R C. Geochemistry and evolution of Iherzolite-bearing phonolitic lavas from Nigeria, Australia, East Germany and New Zealand[J]. Geochimica et Cosmochimica Acta, 1981, 45(8): 1309-1320. DOI URL
[11]	HAY D E, WENDLANDT R F. The origin of Kenya rift plateau-type flood phonolites: results of high-pressure/high-temperature experiments in the systems phonolite-H₂O and phonolite-H₂O-CO₂[J]. Journal of Geophysical Research: Solid Earth, 1995, 100(B1): 401-410.
[12]	KASZUBA J P, WENDLANDT R F. Effect of carbon dioxide on dehydration melting reactions and melt compositions in the lower crust and the origin of alkaline rocks[J]. Journal of Petrology, 2000, 41(3): 363-386. DOI URL
[13]	LEGENDRE C, MAURY R C, CAROFF M, et al. Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): partial melting of basanites followed by crustal contamination[J]. Journal of Petrology, 2005, 46(9): 1925-1962. DOI URL
[14]	BEARD C D, GOODENOUGH K M, BORST A M, et al. Alkaline-silicate REE-HFSE systems[J]. Economic Geology, 2023, 118(1): 177-208. DOI URL
[15]	ZHU S Z, HUANG X L, YU Y, et al. Enrichment of incompatible elements in alkaline syenites in large igneous provinces due to magma replenishment and reactive porous flow in a mush reservoir[J]. Journal of Petrology, 2023, 64(2): egad002.
[16]	WU M Q, et al. The giant Baerzhe rare-earth-element-Nb-Zr-Be deposit, Inner Mongolia, China, an Early Cretaceous analogue of the Strange Lake rare-metal deposit, Quebec[J]. Geological Society, London, Special Publications, 2025, 551(1): 341-353. DOI URL
[17]	WU M Q, SAMSON I M, QIU K F, et al. Multi-stage metasomatic Zr mineralization in the world-class Baerzhe rare earth element Nb-Zr-Be deposit, China[J]. American Mineralogist, 2023, 108(2): 389-405. DOI URL
[18]	WU M Q, SAMSON I M, QIU K F, et al. Concentration mechanisms of rare earth element-Nb-Zr-Be mineralization in the Baerzhe deposit, Northeast China: insights from textural and chemical features of amphibole and rare metal minerals[J]. Economic Geology, 2021, 116(3): 651-679. DOI URL
[19]	YANG W B, NIU H C, SHAN Q, et al. Geochemistry of magmatic and hydrothermal zircon from the highly evolved Baerzhe alkaline granite: implications for Zr-REE-Nb mineralization[J]. Mineralium Deposita, 2014, 49(4): 451-470. DOI URL
[20]	MÖLLER V, WILLIAMS-JONES A E. Petrogenesis of the Nechalacho Layered Suite, Canada: magmatic evolution of a REE-Nb-rich nepheline syenite intrusion[J]. Journal of Petrology, 2016, 57(2): 229-276. DOI URL
[21]	KOGARKO L N. Ore-forming potential of alkaline magmas[J]. Lithos, 1990, 26(1/2): 167-175. DOI URL
[22]	KOGARKO L N, LAHAYE Y, BREY G P. Plume-related mantle source of super-large rare metal deposits from the Lovozero and Khibina massifs on the Kola Peninsula, eastern part of Baltic Shield: Sr, Nd and Hf isotope systematics[J]. Mineralogy and Petrology, 2010, 98(1): 197-208. DOI URL
[23]	CARLSON R W, PEARSON D G, JAMES D E. Physical, chemical, and chronological characteristics of continental mantle[J]. Reviews of Geophysics, 2005, 43: 2004RG000156.
[24]	KUSKY T M, POLAT A, WINDLEY B F, et al. Insights into the tectonic evolution of the North China Craton through comparative tectonic analysis: a record of outward growth of Precambrian continents[J]. Earth-Science Reviews, 2016, 162: 387-432. DOI URL
[25]	ZHAO G C, CAWOOD P A. Precambrian geology of China[J]. Precambrian Research, 2012, 222/223: 13-54. DOI URL
[26]	ZHAO G C, WILDE S A, CAWOOD P A, et al. Archean blocks and their boundaries in the North China Craton: lithological, geochemical, structural and P-T path constraints and tectonic evolution[J]. Precambrian Research, 2001, 107(1/2): 45-73. DOI URL
[27]	QIU K-F, GOLDFARB R J, DENG J, et al. Chapter 35: gold deposits of the Jiaodong Peninsula, eastern China[M]// Geology of the world’s major gold deposits and provinces. Littleton: Society of Economic Geologists, 2020: 753-774.
[28]	DENG J, WANG Q F. Gold mineralization in China: metallogenic provinces, deposit types and tectonic framework[J]. Gondwana Research, 2016, 36: 219-274. DOI URL
[29]	XU Y G. Thermo-tectonic destruction of the Archaean lithospheric keel beneath the Sino-Korean Craton in China: evidence, timing and mechanism[J]. Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy, 2001, 26(9/10): 747-757. DOI URL
[30]	朱日祥, 陈凌, 吴福元, 等. 华北克拉通破坏的时间, 范围与机制[J]. 中国科学: 地球科学, 2011, 41(5): 583-592.
[31]	郑永飞, 徐峥, 赵子福, 等. 华北中生代镁铁质岩浆作用与克拉通减薄和破坏[J]. 中国科学: 地球科学, 2018, 48(4): 379-414.
[32]	WU F-Y, YANG J-H, XU Y-G, et al. Destruction of the North China Craton in the Mesozoic[J]. Annual Review of Earth and Planetary Sciences, 2019, 47: 173-195. DOI URL
[33]	DENG J, YANG L-Q, GROVES D I, et al. An integrated mineral system model for the gold deposits of the giant Jiaodong province, Eastern China[J]. Earth-Science Reviews, 2020, 208: 103274. DOI URL
[34]	HUANG X L, ZHONG J W, XU Y G. Two tales of the continental lithospheric mantle prior to the destruction of the North China Craton: insights from Early Cretaceous mafic intrusions in western Shandong, East China[J]. Geochimica et Cosmochimica Acta, 2012, 96: 193-214. DOI URL
[35]	汤艳杰, 英基丰, 赵月鹏, 等. 华北克拉通岩石圈地幔特征与演化过程[J]. 中国科学: 地球科学, 2021, 51(9): 1489-1503.
[36]	CHENG L, CHENG C, WEI Z. Contrasting structural features at different boundary areas of the North China craton and its tectonic implications[J]. Advances in Earth Science, 2010, 25(6): 571.
[37]	杨进辉, 许蕾, 孙金凤, 等. 华北克拉通破坏与岩浆-成矿的深部动力学过程[J]. 中国科学: 地球科学, 2021, 51(9): 1401-1419.
[38]	张剑, 李三忠, 李玺瑶, 等. 鲁西地区燕山期构造变形: 古太平洋板块俯冲的构造响应[J]. 地学前缘, 2017, 24(4): 226-238. DOI
[39]	LAN J, LI D, XING N, et al. Petrogenesis of the alkaline complex in the Weishan REE deposit, Luxi block, eastern North China Craton: implications for REE mineralization[J]. Ore Geology Reviews, 2024, 167: 106005. DOI URL
[40]	LAN T G, FAN H R, HU F F, et al. Multiple crust-mantle interactions for the destruction of the North China Craton: geochemical and Sr-Nd-Pb-Hf isotopic evidence from the Longbaoshan alkaline complex[J]. Lithos, 2011, 122(1/2): 87-106. DOI URL
[41]	YANG Z Y, LI S S, AN M G, et al. Petrogenesis of alkaline complex of the Longbaoshan rare earth element deposit in the Luxi block, North China Craton, China[J]. Minerals, 2022, 12(12): 1524.
[42]	ZHANG H F, SUN M, ZHOU X H, et al. Geochemical constraints on the origin of Mesozoic alkaline intrusive complexes from the North China Craton and tectonic implications[J]. Lithos, 2005, 81(1/2/3/4): 297-317. DOI URL
[43]	WEI P F, LI D P, SONG Z G, et al. Petrogenesis and relationship with REE mineralization of the quartz syenite from Chishan and Longbaoshan alkaline complex, southeastern North China Craton: insights from zircon U-Pb geochronology, element, and Sr-Nd-Pb-Hf isotope geochemistry[J]. Frontiers in Earth Science, 2023, 10: 1046071. DOI URL
[44]	周伟伟. 郯庐断裂带晚中生代富碱侵入岩年代学, 岩石地球化学及其地质意义[D]. 北京: 中国地质大学(北京), 2014.
[45]	ZHANG H F, SUN M, ZHOU X H, et al. Mesozoic lithosphere destruction beneath the North China Craton: evidence from major-, trace-element and Sr-Nd-Pb isotope studies of Fangcheng basalts[J]. Contributions to Mineralogy and Petrology, 2002, 144(2): 241-254. DOI URL
[46]	WANG C, LIU J C, ZHANG H D, et al. Geochronology and mineralogy of the Weishan carbonatite in Shandong Province, eastern China[J]. Geoscience Frontiers, 2019, 10(2): 769-785. DOI URL
[47]	尚振, 赵超, 支成龙, 等. 鲁西龙宝山稀土矿重稀土矿体的发现及其勘查意义[J]. 地质通报, 2024, 43(增刊1): 484-488.
[48]	兰君, 刘晓, 张鹏, 等. 山东微山稀土矿床成因研究: 稀土矿物学约束[J]. 现代地质, 2025, 39(3): 612-627.
[49]	王继芳, 徐然, 安茂国, 等. 山东省龙宝山地区稀土矿成矿地质特征及找矿前景分析[J]. 山东国土资源, 2020, 36(12): 1-12.
[50]	YANG Z Y, WU M Q, LI S S, et al. The origin of glimmerite and its significance to rare earth element mineralization: insights from the Longbaoshan deposit in North China Craton[J]. Ore Geology Reviews, 2025, 184: 106698. DOI URL
[51]	牛树银, 胡华斌, 毛景文, 等. 鲁西地区地层(岩石)展布及其成因[J]. 地学前缘, 2003, 10(4): 371-372.
[52]	GUO P, SANTOSH M, LI S R. Geodynamics of gold metallogeny in the Shandong Province, NE China: an integrated geological, geophysical and geochemical perspective[J]. Gondwana Research, 2013, 24(3/4): 1172-1202. DOI URL
[53]	QIU J S, CHING-HUA L O, MCINNES B I A, et al. Potash-rich magmatism and associated gold-copper mineralization in the Yishu deep fault zone and its vicinity, eastern China[J]. Resource Geology, 2000, 50(4): 269-280. DOI URL
[54]	DENG J, WANG C M, BAGAS L, et al. Crustal architecture and metallogenesis in the south-eastern North China Craton[J]. Earth-Science Reviews, 2018, 182: 251-272. DOI URL
[55]	LAN T G, HU R Z, CHEN Y H, et al. Generation of high-Mg diorites and associated iron mineralization within an intracontinental setting: insights from ore-barren and ore-bearing intrusions in the eastern North China Craton[J]. Gondwana Research, 2019, 72: 97-119. DOI URL
[56]	DING C W, ZHAO B C, DAI P, et al. Geochronology, geochemistry and Sr-Nd-Pb-Hf isotopes of the alkaline-carbonatite complex in the Weishan REE deposit, Luxi block: constraints on the genesis and tectonic setting of the REE mineralization[J]. Ore Geology Reviews, 2022, 147: 104996. DOI URL
[57]	ZHAO L Y, LAN T G, FAN H R, et al. Origin and mineralization processes of REE during magmatic-hydrothermal evolution: insights from in situ geochemistry of calcite from the Weishan REE deposit, eastern North China Craton[J]. Ore Geology Reviews, 2023, 162: 105676. DOI URL
[58]	LIN J, LIU Y S, YANG Y H, et al. Calibration and correction of LA-ICP-MS and LA-MC-ICP-MS analyses for element contents and isotopic ratios[J]. Solid Earth Sciences, 2016, 1(1): 5-27. DOI URL
[59]	ZHANG W, HU Z C, LIU Y S. Iso-Compass: new freeware software for isotopic data reduction of LA-MC-ICP-MS[J]. Journal of Analytical Atomic Spectrometry, 2020, 35(6): 1087-1096. DOI URL
[60]	ZHANG W, HU Z C. Estimation of isotopic reference values for pure materials and geological reference materials[J]. Atomic Spectroscopy, 2020, 41(3): 93-102. DOI URL
[61]	LI J, TANG S H, ZHU X K, et al. Production and certification of the reference material GSB 04-3258-2015 as a ¹⁴³Nd/¹⁴⁴Nd isotope ratio reference[J]. Geostandards and Geoanalytical Research, 2017, 41(2): 255-262. DOI URL
[62]	SUN S S, McDONOUGH W F. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes[J]. Geological Society, London, Special Publications, 1989, 42(1): 313-345. DOI URL
[63]	LIU Y, WEI J H, ZHANG D H, et al. Early Cretaceous Wulong intermediate-mafic dike swarms in the Liaodong Peninsula: implications for rapid lithospheric delamination of the North China Craton[J]. Lithos, 2020, 362/363: 105473. DOI URL
[64]	赛盛勋, 赵天明, 王中亮, 等. 玲珑黑云母花岗岩成因: 矿物学特征约束[J]. 岩石学报, 2016, 32(8): 2477-2493.
[65]	周予茜, 时毓, 黄椿文, 等. 桂东南莲垌和古龙岩体加里东期I型花岗岩类的岩石成因及构造意义[J]. 地学前缘, 2024, 31(2): 224-248. DOI
[66]	JAHN B M, AUVRAY B, SHEN Q H, et al. Archean crustal evolution in China: the Taishan complex, and evidence for juvenile crustal addition from long-term depleted mantle[J]. Precambrian Research, 1988, 38(4): 381-403. DOI URL
[67]	JAHN B M, WU F Y, LO C H, et al. Crust-mantle interaction induced by deep subduction of the continental crust: geochemical and Sr-Nd isotopic evidence from post-collisional mafic-ultramafic intrusions of the northern Dabie complex, Central China[J]. Chemical Geology, 1999, 157(1/2): 119-146. DOI URL
[68]	ELLIOTT T. Tracers of the slab[M]//Inside the subduction factory. Washington, D. C.: American Geophysical Union, 2003: 23-45.
[69]	MA L T, DAI L Q, ZHENG Y F, et al. Trace elements and Li isotopes distinguish between liquid and solid phases contributing to mafic arc magmas[J]. Lithos, 2023, 454/455: 107232. DOI URL
[70]	WU H H, HUANG H, ZHANG Z C, et al. Highly differentiated trachytic magma linked with rare metal mineralization: a case study from the Shuanghekou Nb deposit, South Qinling[J]. Lithos, 2023, 438/439: 106990. DOI URL
[71]	FOLEY S F, VENTURELLI G, GREEN D H, et al. The ultrapotassic rocks: characteristics, classification, and constraints for petrogenetic models[J]. Earth-Science Reviews, 1987, 24(2): 81-134. DOI URL
[72]	徐义刚, 王强, 唐功建, 等. 弧玄武岩的成因: 进展与问题[J]. 中国科学: 地球科学, 2020, 50(12): 27.
[73]	PILET S, BAKER M B, MÜNTENER O, et al. Monte Carlo simulations of metasomatic enrichment in the lithosphere and implications for the source of alkaline basalts[J]. Journal of Petrology, 2011, 52(7/8): 1415-1442. DOI URL
[74]	FOLEY S F, JACKSON S E, FRYER B J, et al. Trace element partition coefficients for clinopyroxene and phlogopite in an alkaline lamprophyre from Newfoundland by LAM-ICP-MS[J]. Geochimica et Cosmochimica Acta, 1996, 60(4): 629-638. DOI URL
[75]	GREEN T H. Experimental studies of trace-element partitioning applicable to igneous petrogenesis: Sedona 16 years later[J]. Chemical Geology, 1994, 117(1/2/3/4): 0009254194901198.
[76]	ZHOU Y, ZHOU J X, WANG M, et al. A genetic linkage between refertilized mantle and REE enrichment in an alkaline-silicate system: a case of nepheline syenite in the Gejiu district, SW China[J]. Lithos, 2024, 470/471: 107533. DOI URL
[77]	ZHU Y S, YANG J H, SUN J F, et al. Petrogenesis of coeval silica-saturated and silica-undersaturated alkaline rocks: mineralogical and geochemical evidence from the Saima alkaline complex, NE China[J]. Journal of Asian Earth Sciences, 2016, 117: 184-207. DOI URL
[78]	SUN H, XIAO Y L, GAO Y J, et al. Fluid and melt inclusions in the Mesozoic Fangcheng basalt from North China Craton: implications for magma evolution and fluid/melt-peridotite reaction[J]. Contributions to Mineralogy and Petrology, 2013, 165(5): 885-901. DOI URL
[79]	ZHANG H F. Transformation of lithospheric mantle through peridotite-melt reaction: a case of Sino-Korean Craton[J]. Earth and Planetary Science Letters, 2005, 237(3/4): 768-780. DOI URL
[80]	YANG W B, NIU H C, SHAN Q, et al. Geochemistry of primary-carbonate bearing K-rich igneous rocks in the Awulale Mountains, western Tianshan: implications for carbon-recycling in subduction zone[J]. Geochimica et Cosmochimica Acta, 2014, 143: 143-164. DOI URL
[81]	YANG W B, NIU H C, HOLLINGS P, et al. The role of recycled oceanic crust in the generation of alkaline A-type granites[J]. Journal of Geophysical Research: Solid Earth, 2017, 122(12): 9775-9783. DOI URL
[82]	ZHAO Z D, MO X X, DILEK Y, et al. Geochemical and Sr-Nd-Pb-O isotopic compositions of the post-collisional ultrapotassic magmatism in SW Tibet: petrogenesis and implications for India intra-continental subduction beneath southern Tibet[J]. Lithos, 2009, 113(1/2): 190-212. DOI URL
[83]	ZHANG H F, SUN M. Geochemistry of Mesozoic basalts and mafic dikes, southeastern North China Craton, and tectonic implications[J]. International Geology Review, 2002, 44(4): 370-382. DOI URL
[84]	YANG D B, XU W L, PEI F P, et al. Spatial extent of the influence of the deeply subducted South China Block on the southeastern North China Block: constraints from Sr-Nd-Pb isotopes in Mesozoic mafic igneous rocks[J]. Lithos, 2012, 136/137/138/139: 246-260.
[85]	YANG Q L, ZHAO Z F, ZHENG Y F. Slab-mantle interaction in continental subduction channel: geochemical evidence from Mesozoic gabbroic intrusives in southeastern North China[J]. Lithos, 2012, 155: 442-460. DOI URL
[86]	DAI F Q, ZHAO Z F, ZHENG Y F, et al. The geochemical nature of mantle sources for two types of Cretaceous basaltic rocks from Luxi and Jiaodong in east-central China[J]. Lithos, 2019, 344/345: 409-424. DOI URL
[87]	许文良, 王清海, 王冬艳, 等. 华北克拉通东部中生代岩石圈减薄的过程与机制: 中生代火成岩和深源捕虏体证据[J]. 地学前缘, 2004, 11(3): 309-317.
[88]	ZHENG Y F, FU B, GONG B, et al. Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie-Sulu orogen in China: implications for geodynamics and fluid regime[J]. Earth-Science Reviews, 2003, 62(1/2): 105-161. DOI URL
[89]	XU H J, ZHANG J F, WANG Y F, et al. Late Triassic alkaline complex in the Sulu UHP terrane: implications for post-collisional magmatism and subsequent fractional crystallization[J]. Gondwana Research, 2016, 35: 390-410. DOI URL
[90]	ZHAO Z F, ZHENG Y F, ZHANG J, et al. Syn-exhumation magmatism during continental collision: evidence from alkaline intrusives of Triassic age in the Sulu orogen[J]. Chemical Geology, 2012, 328: 70-88. DOI URL
[91]	ZHU R X, XU Y G. The subduction of the West Pacific Plate and the destruction of the North China Craton[J]. Science China Earth Sciences, 2019, 62(9): 1340-1350. DOI
[92]	XIA Q K, LIU J, LIU S C, et al. High water content in Mesozoic primitive basalts of the North China Craton and implications on the destruction of cratonic mantle lithosphere[J]. Earth and Planetary Science Letters, 2013, 361: 85-97. DOI URL
[93]	LIU J G, CAI R H, PEARSON D G, et al. Thinning and destruction of the lithospheric mantle root beneath the North China Craton: a review[J]. Earth-Science Reviews, 2019, 196: 102873. DOI URL
[94]	李光洁, 陈永清, 尚志, 等. 扬子地块西缘峨山新元古代高分异I型花岗岩地球化学特征及岩石成因[J]. 地学前缘, 2024, 31(3): 20-39. DOI
[95]	赖绍聪, 杨航, 张方毅. 南秦岭早古生代碱性岩地球化学特征及其成因机制: 研究进展与展望[J]. 地质学报, 2024, 98(3): 799-828.
[96]	LOUCKS R R. Distinctive composition of copper-ore-forming arcmagmas[J]. Australian Journal of Earth Sciences, 2014, 61(1): 5-16. DOI URL
[97]	CABERO M T, MECOLETA S, LÓPEZ-MORO F J. OPTIMASBA: a Microsoft Excel workbook to optimise the mass-balance modelling applied to magmatic differentiation processes and subsolidus overprints[J]. Computers & Geosciences, 2012, 42: 206-211. DOI URL
[98]	ANENBURG M, MAVROGENES J A, BENNETT V C. The fluorapatite P-REE-Th vein deposit at Nolans Bore: genesis by carbonatite metasomatism[J]. Journal of Petrology, 2020, 61: egaa003. DOI URL
[99]	WENG Q, YANG W B, NIU H C, et al. B-Sr-Nd-Pb isotopic constraints on the origin of the Maoniuping alkaline syenite-carbonatite complex, SW China[J]. Ore Geology Reviews, 2021, 135: 104193. DOI URL
[100]	SMITH M P, MOORE K, KAVECSÁNSZKI D, et al. From mantle to critical zone: a review of large and giant sized deposits of the rare earth elements[J]. Geoscience Frontiers, 2016, 7(3): 315-334. DOI URL
[101]	XUE S, LING M X, LIU Y L, et al. Recycling of subducted carbonates: formation of the Taohuala Mountain carbonatite, North China Craton[J]. Chemical Geology, 2018, 478: 89-101. DOI URL
[102]	吴鸣谦, 马甲栋, 邓军, 等. 巴尔哲锆-铌-铍-稀土矿床成矿精细过程研究[J]. 岩石学报, 2024, 40(6): 1817-1836.
[103]	李厚民, 李立兴, 李以科, 等. 内蒙古白云鄂博铁-铌-稀土矿床矿化蚀变矿物组合及流体组成[J]. 现代地质, 2024, 38(1): 13-24.
[104]	冯婷婷, 蔡诗柔, 张振杰. 基于知识图谱的碳酸岩型稀土矿成矿要素挖掘[J]. 地学前缘, 2025, 32(4): 262-279. DOI
[105]	ZHANG D H, QIU K F, BEARD C D, et al. Amphiboles of the rare earth element-rich Baerzhe peralkaline granite, Northeast China: recorders of fluoride-silicate melt immiscibility and rare metal enrichment[J]. Economic Geology, 2025, 120(2): 475-497. DOI URL
[106]	QIU K F, YU H C, WU M Q, et al. Discrete Zr and REE mineralization of the Baerzhe rare-metal deposit, China[J]. American Mineralogist, 2019, 104(10): 1487-1502. DOI URL
[107]	HAWKESWORTH C. Mantle and slab contribution in arc magmas[J]. Annual Review of Earth and Planetary Sciences, 1993, 21: 175-204. DOI URL
[108]	HAWKESWORTH C J, TURNER S P, MCDERMOTT F, et al. U-Th isotopes in arc magmas: implications for element transfer from the subducted crust[J]. Science, 1997, 276(5312): 551-555. PMID
[109]	GRIFFIN W L, BEGG G C, O’REILLY S Y. Continental-root control on the genesis of magmatic ore deposits[J]. Nature Geoscience, 2013, 6(11): 905-910. DOI
[110]	HOU Z Q, LIU Y, TIAN S H, et al. Formation of carbonatite-related giant rare-earth-element deposits by the recycling of marine sediments[J]. Scientific Reports, 2015, 5: 10231. DOI PMID
[111]	QIU K F, DENG J, LI S S, et al. Roles and perspectives of A- and I-type magmas in rare earth element and gold mineralization[J]. GSA Bulletin, 2023, 136(3/4): 1238-1250.
[112]	SALTERS V J M, STRACKE A. Composition of the depleted mantle[J]. Geochemistry, Geophysics, Geosystems, 2004, 5(5): 2003GC000597.
[113]	PLANK T, LANGMUIR C H. The chemical composition of subducting sediment and its consequences for the crust and mantle[J]. Chemical Geology, 1998, 145(3/4): 325-394. DOI URL
[114]	KATO Y, FUJINAGA K, NAKAMURA K, et al. Deep-sea mud in the Pacific Ocean as a potential resource for rare-earth elements[J]. Nature Geoscience, 2011, 4(8): 535-539. DOI
[115]	张东, 杨武斌, 牛贺才. 钠交代作用对碱性花岗岩体系中稀土富集成矿的贡献[J]. 岩石学报, 2024, 40(3): 864-872.
[116]	马甲栋, 吴鸣谦, 刁习, 等. 钠化和赤铁矿化蚀变对Zr和Nb-Be-REE矿化的指示意义: 以内蒙古巴尔哲矿床为例[J]. 岩石学报, 2023, 39(2): 432-444.
[117]	HÖVELMANN J, PUTNIS A, GEISLER T, et al. The replacement of plagioclase feldspars by albite: observations from hydrothermal experiments[J]. Contributions to Mineralogy and Petrology, 2010, 159(1): 43-59. DOI URL
[118]	徐晶晶, 李林, 杨小男. 稀土元素对褐帘石晶体结构的精细影响研究[J]. 现代地质, 2025, 39(3): 704-714.

样品编号	岩性	钻孔孔号	取样深度/m
LZK701-11	正长斑岩	LZK701	79.8
LZK701-12	正长斑岩	LZK701	85.4
LZK701-13	正长斑岩	LZK701	92.0
LZK701-14	正长斑岩	LZK701	98.1
LZK702-2	正长斑岩	LZK702	195.0
LZK702-3	正长斑岩	LZK702	199.5
LZK702-4	正长斑岩	LZK702	202.7
LZK602-3	石英正长斑岩	LZK602	89.0
LZK602-5	石英正长斑岩	LZK602	102.3
LZK602-6	石英正长斑岩	LZK602	106.0
LZK602-7	石英正长斑岩	LZK602	109.5
LZK602-8	石英正长斑岩	LZK602	111.8
LZK602-10	石英正长斑岩	LZK602	118.9
LZK602-11	石英正长斑岩	LZK602	122.0
LZK701-8	含角闪正长斑岩	LZK701	62.1
LZK701-9	含角闪正长斑岩	LZK701	69.4
LZK701-10	含角闪正长斑岩	LZK701	74.9
LZK602-9	含角闪正长斑岩	LZK602	115.6

样品编号	岩性	钻孔孔号	取样深度/m
LZK701-11	正长斑岩	LZK701	79.8
LZK701-12	正长斑岩	LZK701	85.4
LZK701-13	正长斑岩	LZK701	92.0
LZK701-14	正长斑岩	LZK701	98.1
LZK702-2	正长斑岩	LZK702	195.0
LZK702-3	正长斑岩	LZK702	199.5
LZK702-4	正长斑岩	LZK702	202.7
LZK602-3	石英正长斑岩	LZK602	89.0
LZK602-5	石英正长斑岩	LZK602	102.3
LZK602-6	石英正长斑岩	LZK602	106.0
LZK602-7	石英正长斑岩	LZK602	109.5
LZK602-8	石英正长斑岩	LZK602	111.8
LZK602-10	石英正长斑岩	LZK602	118.9
LZK602-11	石英正长斑岩	LZK602	122.0
LZK701-8	含角闪正长斑岩	LZK701	62.1
LZK701-9	含角闪正长斑岩	LZK701	69.4
LZK701-10	含角闪正长斑岩	LZK701	74.9
LZK602-9	含角闪正长斑岩	LZK602	115.6

样品编号	岩性	主量元素含量/%																																																A/CNK				A/NK
样品编号	岩性	SiO₂				TiO₂				Al₂O₃				TFeO				MnO				MgO				CaO				Na₂O				K₂O				P₂O₅				LOI				Na₂O+ K₂O				A/CNK				A/NK
LZK602-3	石英正长斑岩	62.4				0.24				14.6				2.68				0.05				0.70				1.77				5.68				4.43				0.20				3.44				10.11				0.84				1.03
LZK602-5		65.1				0.14				15.5				2.53				0.05				0.38				1.32				5.61				5.58				0.07				3.16				11.19				0.88				1.02
LZK602-6		65.6				0.16				15.8				1.99				0.05				0.33				1.28				5.91				4.98				0.07				1.21				10.89				0.91				1.05
LZK602-7		63.0				0.17				14.7				2.22				0.05				0.57				1.76				5.02				5.44				0.09				1.56				10.46				0.85				1.04
LZK602-8		68.0				0.19				15.2				1.99				0.04				0.37				1.31				5.84				4.69				0.10				0.33				10.53				0.89				1.04
LZK602-10		66.3				0.21				14.4				2.63				0.10				1.61				1.58				5.23				4.72				0.10				1.82				9.95				0.87				1.05
LZK602-11		60.9				0.51				16.6				4.12				0.09				1.53				2.98				6.42				3.81				0.43				1.27				10.23				0.83				1.13
LZK701-8	含角闪正长斑岩	64.0				0.22				13.6				3.04				0.06				0.46				2.19				6.23				4.06				0.15				2.67				10.29				0.73				0.93
LZK701-9		67.5				0.19				12.9				3.10				0.03				0.80				0.52				6.32				3.79				0.10				0.57				10.11				0.84				0.89
LZK701-10		66.5				0.19				13.4				2.92				0.04				0.69				0.94				6.04				4.04				0.11				0.51				10.08				0.84				0.94
LZK602-9		65.7				0.32				15.1				2.63				0.11				1.17				1.83				6.48				5.01				0.20				0.65				11.49				0.78				0.94
样品编号	岩性	微量元素含量/10^-6
样品编号	岩性	Li	Be				Sc				V				Cr				Ni				Co				Cu				Zn				Ga				Rb				Sr				Y				Zr			Nb
LZK602-3	石英正长斑岩	11.6	3.62				1.55				36.3				6.3				7.60				4.36				42.6				20.6				33.1				114				803				17.8				401			17.1
LZK602-5		7.17	4.09				1.23				15.8				3.38				5.00				4.68				48.8				24.0				29.5				139				479				16.6				456			26.7
LZK602-6		10.4	4.52				1.21				19.8				5.05				4.70				2.16				9.70				28.3				32.7				127				887				15.9				492			28.6
LZK602-7		10.1	4.05				1.18				24.3				3.48				6.40				3.30				36.4				22.6				34.7				147				499				16.5				433			25.7
LZK602-8		11.2	4.34				0.85				25.6				3.50				6.20				3.06				10.9				17.1				32.0				122				775				13.4				475			26.8
LZK602-10		57.9	4.24				1.25				25.3				7.25				6.70				4.63				43.2				87.8				38.6				179				1 053				32.6				376			22.6
LZK602-11		31.4	3.48				5.68				62.4				16.6				10.5				7.67				20.6				37.8				30.9				117				2 290				19.8				714			20.6
LZK701-8	含角闪正长斑岩	67.3	4.52				2.05				50.5				24.7				18.2				28.4				189				40.3				33.5				116				408				19.2				319			17.3
LZK701-9		60.8	6.43				2.02				36.8				14.3				14.6				4.62				70.4				72.0				37.1				127				606				18.8				396			29.2
LZK701-10		48.5	5.15				1.76				32.7				16.9				13.3				5.55				85.3				85.4				33.8				124				522				17.7				410			33.2
LZK602-9		25.6	8.11				3.47				33.8				41.4				16.8				5.93				5.00				62.5				28.3				104				1 343				23.4				545			59.8
样品编号	岩性	微量元素含量/10^-6
样品编号	岩性	Cs	Ba				La				Ce				Pr				Nd				Sm				Eu				Gd				Tb				Dy				Ho				Er				Tm			Yb
LZK602-3	石英正长斑岩	0.66	3 120				196				338				35.1				104				12.7				3.02				10.0				0.91				3.96				0.57				1.31				0.17			0.75
LZK602-5		0.79	2 167				162				274				28.9				85				10.8				2.73				8.60				0.83				3.47				0.53				1.24				0.17			0.90
LZK602-6		0.86	2 324				168				287				29.7				87				10.8				2.62				8.40				0.81				3.45				0.53				1.22				0.18			0.86
LZK602-7		1.68	2 182				195				323				32.6				97				11.3				2.87				9.20				0.85				3.56				0.56				1.26				0.18			0.98
LZK602-8		0.92	2 342				163				280				29.4				86				10.1				2.58				8.10				0.76				3.07				0.46				1.05				0.16			0.83
LZK602-10		1.68	2 170				306				544				55.2				163				19.7				4.78				15.5				1.49				6.55				0.98				2.27				0.27			1.23
LZK602-11		2.33	3 913				278				424				40.8				132				14.7				3.62				8.50				1.07				4.14				0.73				2.12				0.28			1.87
LZK701-8	含角闪正长斑岩	0.47	1 296				212				331				33.7				100				12.5				3.01				9.70				0.92				4.01				0.64				1.39				0.17			0.79
LZK701-9		0.73	1 557				211				345				34.5				101				12.1				2.57				9.40				0.89				3.92				0.59				1.47				0.19			1.13
LZK701-10		0.69	1 512				170				280				28.3				84				10.6				2.41				8.10				0.79				3.57				0.58				1.32				0.17			0.82
LZK602-9		0.36	2 369				132				229				21.5				74				10.4				2.44				7.00				0.93				4.05				0.75				2.14				0.32			2.14
样品编号	岩性	微量元素含量/10^-6																													Th/Nb				Th/Yb				Ba/Th				Nb/Y				Th/La				Sm/La			La/Sm
样品编号	岩性	Lu	Hf				Ta				Tl				Pb				Bi				Th				U				Th/Nb				Th/Yb				Ba/Th				Nb/Y				Th/La				Sm/La			La/Sm
LZK602-3	石英正长斑岩	0.13	4.06				0.64				0.54				34.2				0.98				21.6				4.34				1.26				28.80				144.44				0.96				0.11				0.06			15.43
LZK602-5		0.18	4.39				0.90				0.59				28.2				1.05				38.3				14.0				1.43				42.56				56.58				1.61				0.24				0.07			15.00
LZK602-6		0.17	5.08				1.39				0.56				23.4				0.26				34.1				8.63				1.19				39.65				68.15				1.80				0.20				0.06			15.56
LZK602-7		0.18	4.57				0.60				0.65				16.4				0.20				34.7				8.53				1.35				35.41				62.88				1.56				0.18				0.06			17.26
LZK602-8		0.17	4.44				0.92				0.51				18.2				0.20				24.6				6.59				0.92				29.64				95.20				2.00				0.15				0.06			16.14
LZK602-10		0.19	3.86				0.51				0.60				75.5				0.62				29.1				10.4				1.29				23.66				74.57				0.69				0.10				0.06			15.53
LZK602-11		0.31	16.1				1.08				0.72				13.5				0.23				41.4				5.53				2.00				22.13				94.55				1.04				0.15				0.05			18.90
LZK701-8	含角闪正长斑岩	0.13	4.83				0.62				0.38				27.1				0.19				20.0				5.34				1.16				25.32				64.80				0.90				0.09				0.06			16.96
LZK701-9		0.19	5.67				0.83				0.36				21.3				0.10				20.0				5.60				0.68				17.70				77.85				1.55				0.09				0.06			17.44
LZK701-10		0.13	5.75				0.96				0.40				19.4				0.10				20.0				7.35				0.60				24.39				75.60				1.88				0.12				0.06			16.04
LZK602-9		0.33	16.3				3.31				0.57				37.2				0.06				51.0				17.3				0.85				23.86				46.45				2.56				0.39				0.08			12.66
样品编号	岩性	主量元素含量/%																																															A/CNK				A/NK
样品编号	岩性	SiO₂			TiO₂				Al₂O₃				TFeO				MnO				MgO				CaO				Na₂O				K₂O				P₂O₅				LOI				Na₂O+ K₂O				A/CNK				A/NK
LZK701-11	正长斑岩	59.4			0.22				13.5				5.56				0.14				0.96				1.97				3.07				8.10				0.19				4.02				11.17				0.78				0.98
LZK701-12		63.8			0.16				14.0				2.11				0.05				0.72				2.47				5.23				5.04				0.11				2.75				10.27				0.75				1.00
LZK701-13		69.0			0.18				14.7				1.80				0.03				0.76				0.80				5.89				4.77				0.10				0.50				10.66				0.90				0.99
LZK701-14		68.1			0.18				13.9				2.27				0.04				0.69				0.75				6.43				4.31				0.10				0.67				10.74				0.84				0.91
LZK702-2		57.9			0.50				15.4				3.99				0.11				3.44				5.01				5.88				4.10				0.46				2.11				9.98				0.66				1.09
LZK702-3		58.5			0.44				16.2				4.35				0.17				1.96				4.45				5.75				4.58				0.40				1.95				10.32				0.72				1.12
LZK702-4		64.6			0.27				15.9				3.38				0.08				0.68				1.50				5.76				5.98				0.18				0.55				11.74				0.85				0.99
样品编号	岩性	微量元素含量/10^-6
样品编号	岩性	Li		Be				Sc				V				Cr				Ni				Co				Cu				Zn				Ga				Rb				Sr				Y				Zr			Nb
LZK701-11	正长斑岩	15.9		3.36				1.31				63.5				14.3				13.9				5.66				176				119				32.9				206				360				23.5				322			19.8
LZK701-12		32.3		4.94				1.03				23.8				19.4				10.1				3.21				28.6				39.0				34.0				137				482				19.9				365			28.0
LZK701-13		82.4		6.69				1.46				23.8				23.8				13.1				3.83				16.0				37.1				32.5				154				401				20.2				398			31.2
LZK701-14		38.0		8.23				1.49				23.5				12.1				13.1				3.74				19.1				45.0				38.2				129				583				23.1				413			40.4
LZK702-2		60.8		5.14				9.36				75.6				117				75.6				16.4				28.4				109				25.9				82.0				1 892				21.8				311			21.1
LZK702-3		40.8		3.41				5.51				72.5				25.7				13.1				10.9				115				95.0				29.3				98.0				1 324				21.9				73.0			11.4
LZK702-4		34.1		5.17				2.82				31.9				11.2				4.60				4.91				108				33.1				29.0				142				2 128				15.9				550			33.2
样品编号	岩性	微量元素含量/10^-6
样品编号	岩性	Cs		Ba				La				Ce				Pr				Nd				Sm				Eu				Gd				Tb				Dy				Ho				Er				Tm			Yb
LZK701-11	正长斑岩	0.59		2 204				206				359				36.8				109				13.3				3.12				10.1				1.00				4.63				0.71				1.67				0.23			1.13
LZK701-12		0.55		1 940				195				313				31.4				92.0				11.6				2.78				8.90				0.88				3.88				0.60				1.52				0.20			1.08
LZK701-13		0.84		1 471				139				231				24.0				72.0				9.80				2.31				7.70				0.83				3.85				0.63				1.48				0.20			0.96
LZK701-14		0.46		1 389				179				305				31.6				93.0				12.4				2.67				9.60				0.97				4.60				0.70				1.72				0.21			1.24
LZK702-2		0.63		2 869				150				259				26.9				102				14.4				3.81				9.50				1.13				4.58				0.76				2.06				0.26			1.60
LZK702-3		0.90		5 460				184				282				26.2				93.0				12.9				4.14				8.40				1.04				4.26				0.73				1.91				0.24			1.50
LZK702-4		0.81		3 269				230				347				31.0				98.0				11.1				2.93				6.70				0.82				3.14				0.57				1.62				0.23			1.54
样品编号	岩性	微量元素含量/10^-6																														Th/Nb				Th/Yb				Ba/Th				Nb/Y				Th/La				Sm/La			La/Sm
样品编号	岩性	Lu		Hf				Ta				Tl				Pb				Bi				Th				U				Th/Nb				Th/Yb				Ba/Th				Nb/Y				Th/La				Sm/La			La/Sm
LZK701-11	正长斑岩	0.18		4.35				1.53				0.84				37.2				0.10				39.3				11.4				1.98				34.78				56.08				0.84				0.19				0.06			15.49
LZK701-12		0.15		4.72				0.89				0.51				18.5				0.06				35.1				8.46				1.25				32.50				55.27				1.41				0.18				0.06			16.81
LZK701-13		0.14		5.61				2.20				0.46				17.6				0.07				37.3				6.34				1.20				38.85				39.44				1.54				0.27				0.07			14.15
LZK701-14		0.19		6.09				1.26				0.36				22.0				0.13				41.9				5.85				1.04				33.79				33.15				1.75				0.23				0.07			14.44
LZK702-2		0.26		8.19				0.90				0.45				159				0.44				21.5				8.08				1.02				13.45				133.34				0.97				0.14				0.10			10.43
LZK702-3		0.25		2.54				0.68				0.52				20.1				0.05				15.5				3.23				1.36				10.38				351.23				0.52				0.08				0.07			14.30
LZK702-4		0.29		14.0				1.71				0.60				29.2				0.13				46.8				14.6				1.41				30.35				69.89				2.09				0.20				0.05			20.65

样品编号	岩性	主量元素含量/%																																																A/CNK				A/NK
样品编号	岩性	SiO₂				TiO₂				Al₂O₃				TFeO				MnO				MgO				CaO				Na₂O				K₂O				P₂O₅				LOI				Na₂O+ K₂O				A/CNK				A/NK
LZK602-3	石英正长斑岩	62.4				0.24				14.6				2.68				0.05				0.70				1.77				5.68				4.43				0.20				3.44				10.11				0.84				1.03
LZK602-5		65.1				0.14				15.5				2.53				0.05				0.38				1.32				5.61				5.58				0.07				3.16				11.19				0.88				1.02
LZK602-6		65.6				0.16				15.8				1.99				0.05				0.33				1.28				5.91				4.98				0.07				1.21				10.89				0.91				1.05
LZK602-7		63.0				0.17				14.7				2.22				0.05				0.57				1.76				5.02				5.44				0.09				1.56				10.46				0.85				1.04
LZK602-8		68.0				0.19				15.2				1.99				0.04				0.37				1.31				5.84				4.69				0.10				0.33				10.53				0.89				1.04
LZK602-10		66.3				0.21				14.4				2.63				0.10				1.61				1.58				5.23				4.72				0.10				1.82				9.95				0.87				1.05
LZK602-11		60.9				0.51				16.6				4.12				0.09				1.53				2.98				6.42				3.81				0.43				1.27				10.23				0.83				1.13
LZK701-8	含角闪正长斑岩	64.0				0.22				13.6				3.04				0.06				0.46				2.19				6.23				4.06				0.15				2.67				10.29				0.73				0.93
LZK701-9		67.5				0.19				12.9				3.10				0.03				0.80				0.52				6.32				3.79				0.10				0.57				10.11				0.84				0.89
LZK701-10		66.5				0.19				13.4				2.92				0.04				0.69				0.94				6.04				4.04				0.11				0.51				10.08				0.84				0.94
LZK602-9		65.7				0.32				15.1				2.63				0.11				1.17				1.83				6.48				5.01				0.20				0.65				11.49				0.78				0.94
样品编号	岩性	微量元素含量/10^-6
样品编号	岩性	Li	Be				Sc				V				Cr				Ni				Co				Cu				Zn				Ga				Rb				Sr				Y				Zr			Nb
LZK602-3	石英正长斑岩	11.6	3.62				1.55				36.3				6.3				7.60				4.36				42.6				20.6				33.1				114				803				17.8				401			17.1
LZK602-5		7.17	4.09				1.23				15.8				3.38				5.00				4.68				48.8				24.0				29.5				139				479				16.6				456			26.7
LZK602-6		10.4	4.52				1.21				19.8				5.05				4.70				2.16				9.70				28.3				32.7				127				887				15.9				492			28.6
LZK602-7		10.1	4.05				1.18				24.3				3.48				6.40				3.30				36.4				22.6				34.7				147				499				16.5				433			25.7
LZK602-8		11.2	4.34				0.85				25.6				3.50				6.20				3.06				10.9				17.1				32.0				122				775				13.4				475			26.8
LZK602-10		57.9	4.24				1.25				25.3				7.25				6.70				4.63				43.2				87.8				38.6				179				1 053				32.6				376			22.6
LZK602-11		31.4	3.48				5.68				62.4				16.6				10.5				7.67				20.6				37.8				30.9				117				2 290				19.8				714			20.6
LZK701-8	含角闪正长斑岩	67.3	4.52				2.05				50.5				24.7				18.2				28.4				189				40.3				33.5				116				408				19.2				319			17.3
LZK701-9		60.8	6.43				2.02				36.8				14.3				14.6				4.62				70.4				72.0				37.1				127				606				18.8				396			29.2
LZK701-10		48.5	5.15				1.76				32.7				16.9				13.3				5.55				85.3				85.4				33.8				124				522				17.7				410			33.2
LZK602-9		25.6	8.11				3.47				33.8				41.4				16.8				5.93				5.00				62.5				28.3				104				1 343				23.4				545			59.8
样品编号	岩性	微量元素含量/10^-6
样品编号	岩性	Cs	Ba				La				Ce				Pr				Nd				Sm				Eu				Gd				Tb				Dy				Ho				Er				Tm			Yb
LZK602-3	石英正长斑岩	0.66	3 120				196				338				35.1				104				12.7				3.02				10.0				0.91				3.96				0.57				1.31				0.17			0.75
LZK602-5		0.79	2 167				162				274				28.9				85				10.8				2.73				8.60				0.83				3.47				0.53				1.24				0.17			0.90
LZK602-6		0.86	2 324				168				287				29.7				87				10.8				2.62				8.40				0.81				3.45				0.53				1.22				0.18			0.86
LZK602-7		1.68	2 182				195				323				32.6				97				11.3				2.87				9.20				0.85				3.56				0.56				1.26				0.18			0.98
LZK602-8		0.92	2 342				163				280				29.4				86				10.1				2.58				8.10				0.76				3.07				0.46				1.05				0.16			0.83
LZK602-10		1.68	2 170				306				544				55.2				163				19.7				4.78				15.5				1.49				6.55				0.98				2.27				0.27			1.23
LZK602-11		2.33	3 913				278				424				40.8				132				14.7				3.62				8.50				1.07				4.14				0.73				2.12				0.28			1.87
LZK701-8	含角闪正长斑岩	0.47	1 296				212				331				33.7				100				12.5				3.01				9.70				0.92				4.01				0.64				1.39				0.17			0.79
LZK701-9		0.73	1 557				211				345				34.5				101				12.1				2.57				9.40				0.89				3.92				0.59				1.47				0.19			1.13
LZK701-10		0.69	1 512				170				280				28.3				84				10.6				2.41				8.10				0.79				3.57				0.58				1.32				0.17			0.82
LZK602-9		0.36	2 369				132				229				21.5				74				10.4				2.44				7.00				0.93				4.05				0.75				2.14				0.32			2.14
样品编号	岩性	微量元素含量/10^-6																													Th/Nb				Th/Yb				Ba/Th				Nb/Y				Th/La				Sm/La			La/Sm
样品编号	岩性	Lu	Hf				Ta				Tl				Pb				Bi				Th				U				Th/Nb				Th/Yb				Ba/Th				Nb/Y				Th/La				Sm/La			La/Sm
LZK602-3	石英正长斑岩	0.13	4.06				0.64				0.54				34.2				0.98				21.6				4.34				1.26				28.80				144.44				0.96				0.11				0.06			15.43
LZK602-5		0.18	4.39				0.90				0.59				28.2				1.05				38.3				14.0				1.43				42.56				56.58				1.61				0.24				0.07			15.00
LZK602-6		0.17	5.08				1.39				0.56				23.4				0.26				34.1				8.63				1.19				39.65				68.15				1.80				0.20				0.06			15.56
LZK602-7		0.18	4.57				0.60				0.65				16.4				0.20				34.7				8.53				1.35				35.41				62.88				1.56				0.18				0.06			17.26
LZK602-8		0.17	4.44				0.92				0.51				18.2				0.20				24.6				6.59				0.92				29.64				95.20				2.00				0.15				0.06			16.14
LZK602-10		0.19	3.86				0.51				0.60				75.5				0.62				29.1				10.4				1.29				23.66				74.57				0.69				0.10				0.06			15.53
LZK602-11		0.31	16.1				1.08				0.72				13.5				0.23				41.4				5.53				2.00				22.13				94.55				1.04				0.15				0.05			18.90
LZK701-8	含角闪正长斑岩	0.13	4.83				0.62				0.38				27.1				0.19				20.0				5.34				1.16				25.32				64.80				0.90				0.09				0.06			16.96
LZK701-9		0.19	5.67				0.83				0.36				21.3				0.10				20.0				5.60				0.68				17.70				77.85				1.55				0.09				0.06			17.44
LZK701-10		0.13	5.75				0.96				0.40				19.4				0.10				20.0				7.35				0.60				24.39				75.60				1.88				0.12				0.06			16.04
LZK602-9		0.33	16.3				3.31				0.57				37.2				0.06				51.0				17.3				0.85				23.86				46.45				2.56				0.39				0.08			12.66
样品编号	岩性	主量元素含量/%																																															A/CNK				A/NK
样品编号	岩性	SiO₂			TiO₂				Al₂O₃				TFeO				MnO				MgO				CaO				Na₂O				K₂O				P₂O₅				LOI				Na₂O+ K₂O				A/CNK				A/NK
LZK701-11	正长斑岩	59.4			0.22				13.5				5.56				0.14				0.96				1.97				3.07				8.10				0.19				4.02				11.17				0.78				0.98
LZK701-12		63.8			0.16				14.0				2.11				0.05				0.72				2.47				5.23				5.04				0.11				2.75				10.27				0.75				1.00
LZK701-13		69.0			0.18				14.7				1.80				0.03				0.76				0.80				5.89				4.77				0.10				0.50				10.66				0.90				0.99
LZK701-14		68.1			0.18				13.9				2.27				0.04				0.69				0.75				6.43				4.31				0.10				0.67				10.74				0.84				0.91
LZK702-2		57.9			0.50				15.4				3.99				0.11				3.44				5.01				5.88				4.10				0.46				2.11				9.98				0.66				1.09
LZK702-3		58.5			0.44				16.2				4.35				0.17				1.96				4.45				5.75				4.58				0.40				1.95				10.32				0.72				1.12
LZK702-4		64.6			0.27				15.9				3.38				0.08				0.68				1.50				5.76				5.98				0.18				0.55				11.74				0.85				0.99
样品编号	岩性	微量元素含量/10^-6
样品编号	岩性	Li		Be				Sc				V				Cr				Ni				Co				Cu				Zn				Ga				Rb				Sr				Y				Zr			Nb
LZK701-11	正长斑岩	15.9		3.36				1.31				63.5				14.3				13.9				5.66				176				119				32.9				206				360				23.5				322			19.8
LZK701-12		32.3		4.94				1.03				23.8				19.4				10.1				3.21				28.6				39.0				34.0				137				482				19.9				365			28.0
LZK701-13		82.4		6.69				1.46				23.8				23.8				13.1				3.83				16.0				37.1				32.5				154				401				20.2				398			31.2
LZK701-14		38.0		8.23				1.49				23.5				12.1				13.1				3.74				19.1				45.0				38.2				129				583				23.1				413			40.4
LZK702-2		60.8		5.14				9.36				75.6				117				75.6				16.4				28.4				109				25.9				82.0				1 892				21.8				311			21.1
LZK702-3		40.8		3.41				5.51				72.5				25.7				13.1				10.9				115				95.0				29.3				98.0				1 324				21.9				73.0			11.4
LZK702-4		34.1		5.17				2.82				31.9				11.2				4.60				4.91				108				33.1				29.0				142				2 128				15.9				550			33.2
样品编号	岩性	微量元素含量/10^-6
样品编号	岩性	Cs		Ba				La				Ce				Pr				Nd				Sm				Eu				Gd				Tb				Dy				Ho				Er				Tm			Yb
LZK701-11	正长斑岩	0.59		2 204				206				359				36.8				109				13.3				3.12				10.1				1.00				4.63				0.71				1.67				0.23			1.13
LZK701-12		0.55		1 940				195				313				31.4				92.0				11.6				2.78				8.90				0.88				3.88				0.60				1.52				0.20			1.08
LZK701-13		0.84		1 471				139				231				24.0				72.0				9.80				2.31				7.70				0.83				3.85				0.63				1.48				0.20			0.96
LZK701-14		0.46		1 389				179				305				31.6				93.0				12.4				2.67				9.60				0.97				4.60				0.70				1.72				0.21			1.24
LZK702-2		0.63		2 869				150				259				26.9				102				14.4				3.81				9.50				1.13				4.58				0.76				2.06				0.26			1.60
LZK702-3		0.90		5 460				184				282				26.2				93.0				12.9				4.14				8.40				1.04				4.26				0.73				1.91				0.24			1.50
LZK702-4		0.81		3 269				230				347				31.0				98.0				11.1				2.93				6.70				0.82				3.14				0.57				1.62				0.23			1.54
样品编号	岩性	微量元素含量/10^-6																														Th/Nb				Th/Yb				Ba/Th				Nb/Y				Th/La				Sm/La			La/Sm
样品编号	岩性	Lu		Hf				Ta				Tl				Pb				Bi				Th				U				Th/Nb				Th/Yb				Ba/Th				Nb/Y				Th/La				Sm/La			La/Sm
LZK701-11	正长斑岩	0.18		4.35				1.53				0.84				37.2				0.10				39.3				11.4				1.98				34.78				56.08				0.84				0.19				0.06			15.49
LZK701-12		0.15		4.72				0.89				0.51				18.5				0.06				35.1				8.46				1.25				32.50				55.27				1.41				0.18				0.06			16.81
LZK701-13		0.14		5.61				2.20				0.46				17.6				0.07				37.3				6.34				1.20				38.85				39.44				1.54				0.27				0.07			14.15
LZK701-14		0.19		6.09				1.26				0.36				22.0				0.13				41.9				5.85				1.04				33.79				33.15				1.75				0.23				0.07			14.44
LZK702-2		0.26		8.19				0.90				0.45				159				0.44				21.5				8.08				1.02				13.45				133.34				0.97				0.14				0.10			10.43
LZK702-3		0.25		2.54				0.68				0.52				20.1				0.05				15.5				3.23				1.36				10.38				351.23				0.52				0.08				0.07			14.30
LZK702-4		0.29		14.0				1.71				0.60				29.2				0.13				46.8				14.6				1.41				30.35				69.89				2.09				0.20				0.05			20.65

样品编号	主量元素含量/%							阳离子数						An	Ab	Or
样品编号	SiO₂	Al₂O₃	FeO	CaO	Na₂O	K₂O	总计	Si	Al	Fe²⁺	Ca	Na	K	An	Ab	Or
22b5-3-1	64.08	18.58	bdl	0.02	0.42	15.90	99.00	11.938	4.079	bdl	0.003	0.153	3.779	0.10	3.90	96.00
22b5-3-2	65.94	19.22	0.30	0.05	4.63	9.95	100.08	11.919	4.095	0.045	0.009	1.621	2.293	0.20	41.30	58.40
22b5-3-3	65.59	18.79	0.33	0.02	1.31	15.18	101.22	11.946	4.034	0.051	0.004	0.461	3.528	0.10	11.50	88.30
22b5-3-4	67.17	19.86	0.29	0.17	11.14	0.46	99.08	11.871	4.136	0.043	0.032	3.815	0.104	0.80	96.50	2.60
22b5-3-5	68.86	19.21	0.37	0.02	11.73	0.18	100.36	12.005	3.947	0.054	0.003	3.964	0.039	0.10	98.90	1.00
22b5-3-6	64.65	18.70	0.29	bdl	0.97	15.69	100.31	11.917	4.063	0.045	bdl	0.346	3.690	bdl	8.60	91.40
22b5-3-7	63.39	20.09	0.48	bdl	0.41	15.27	99.63	11.717	4.376	0.074	bdl	0.147	3.599	bdl	3.90	96.10
22b5-3-8	58.84	23.02	1.52	0.04	0.35	14.45	98.21	11.113	5.124	0.240	0.007	0.129	3.481	0.20	3.60	96.20
22b5-3-9	64.42	18.85	0.18	0.03	0.52	15.90	99.90	11.915	4.110	0.028	0.007	0.186	3.752	0.20	4.70	95.10
22b5-3-10	64.70	19.62	0.29	0.75	5.34	9.12	99.82	11.752	4.201	0.045	0.145	1.881	2.113	3.50	45.40	51.10
22b3-2-1	64.16	18.35	0.46	0.02	2.57	12.60	98.15	11.952	4.029	0.071	0.005	0.928	2.994	0.10	23.60	76.30
22b3-2-2	68.36	20.14	0.40	0.20	11.14	0.76	101.00	11.873	4.122	0.059	0.037	3.750	0.169	0.90	94.80	4.30
22b3-2-3	67.37	19.48	0.23	0.10	8.08	5.09	100.34	11.937	4.067	0.034	0.018	2.777	1.151	0.50	70.40	29.20
22b3-2-4	66.85	18.93	0.39	0.17	8.31	4.90	99.55	11.957	3.990	0.059	0.032	2.882	1.118	0.80	71.50	27.70
22b3-2-5	67.72	19.43	0.37	0.16	8.19	4.81	100.67	11.954	4.042	0.054	0.030	2.804	1.083	0.80	71.60	27.70
22b3-2-6	62.82	18.60	0.31	0.06	0.49	15.52	97.80	11.878	4.145	0.048	0.013	0.178	3.744	0.30	4.50	95.10
22b3-2-7	62.90	18.42	0.44	0.04	0.49	15.66	97.95	11.889	4.104	0.069	0.008	0.181	3.775	0.20	4.60	95.20
22b3-2-8	62.95	18.55	0.48	0.05	0.49	15.38	97.91	11.880	4.126	0.076	0.011	0.179	3.703	0.30	4.60	95.10
22b3-2-9	62.85	18.55	0.46	0.05	0.53	15.76	98.20	11.861	4.126	0.073	0.010	0.194	3.795	0.20	4.80	94.90
22b3-2-10	67.56	19.21	0.36	0.13	10.13	2.25	99.63	11.958	4.007	0.053	0.024	3.475	0.509	0.60	86.70	12.70
22b3-2-11	67.24	19.24	0.38	0.09	10.47	1.93	99.33	11.930	4.022	0.056	0.016	3.600	0.437	0.40	88.80	10.80
22b3-2-12	64.07	18.33	0.44	0.01	0.93	15.13	98.92	11.945	4.028	0.069	0.002	0.337	3.598	0.10	8.60	91.40
702-1-1	64.22	18.72	0.08	0.02	0.11	16.53	99.68	11.891	4.085	0.012	0.005	0.039	3.904	0.10	1.00	98.90
702-1-2	64.31	18.57	bdl	bdl	0.20	16.51	99.59	11.942	4.063	bdl	bdl	0.072	3.911	bdl	1.80	98.20
702-1-3	65.30	18.92	0.03	bdl	0.03	16.82	101.11	11.948	4.080	0.004	bdl	0.012	3.927	bdl	0.30	99.70
702-1-4	68.56	19.98	0.37	0.03	11.63	0.18	100.75	11.912	4.092	0.054	0.005	3.918	0.039	0.10	98.90	1.00
702-1-5	68.29	19.60	0.35	0.03	11.72	0.18	100.17	11.939	4.039	0.051	0.005	3.974	0.040	0.10	98.90	1.00
702-1-6	63.97	19.21	0.30	0.01	0.45	15.80	99.74	11.850	4.194	0.046	0.002	0.163	3.735	0.05	4.20	95.80
702-1-7	64.68	18.90	0.56	0.02	1.05	15.28	100.49	11.887	4.094	0.086	0.004	0.373	3.582	0.10	9.40	90.50
702-1-8	61.16	18.38	0.03	0.06	0.64	14.54	94.81	11.608	4.110	0.005	0.012	0.235	3.520	0.30	6.20	93.40
702-1-9	64.05	19.24	0.12	bdl	0.82	14.88	99.11	11.849	4.195	0.019	bdl	0.293	3.512	bdl	7.70	92.30
702-1-10	62.82	18.85	0.15	0.03	0.64	14.92	97.41	11.748	4.153	0.023	0.006	0.233	3.560	0.20	6.10	93.70

鲁西地区龙宝山碱性杂岩体岩石成因与稀土元素富集机制

Petrogenesis and rare earth element enrichment of the Longbaoshan alkaline complex, Luxi region

RichHTML

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

图/表 20

参考文献 118

相关文章 15

编辑推荐

Metrics

本文评价

岩性	测年方法	年龄/Ma	数据来源
二长斑岩	全岩Rb-Sr	129.3±4.5	[42]
石英正长斑岩	LA-ICP-MS锆石U-Pb	129.4±0.7	[40]
霓辉正长斑岩	LA-ICP-MS锆石U-Pb	130.1±1.7	[40]
二长斑岩	LA-ICP-MS锆石U-Pb	129.9±0.8	[40]
正长闪长玢岩	LA-ICP-MS锆石U-Pb	131.7±1.4	[40]
角闪正长斑岩	LA-ICP-MS锆石U-Pb	130.1±1.0	[40]
石英正长岩	SHRIMP锆石U-Pb	125±2.2	[44]
角闪闪长岩	LA-ICP-MS榍石U-Pb	120±8.2	[41]
石英正长斑岩	LA-ICP-MS锆石U-Pb	123.7±0.7	[43]

[1]	杜保峰, 李山坡, 吴鸣谦, 张荣臻, 陈俊魁, 王莉, 李珊珊, 邱昆峰. 华北克拉通南缘水磨沟稀土矿床成矿时代及成矿过程[J]. 地学前缘, 2026, 33(2): 247-264.
[2]	李金明, 张杨, 成秋明. 基于机器学习与垂向分层建模联合驱动的华北克拉通地温梯度空间分布预测[J]. 地学前缘, 2025, 32(4): 291-302.
[3]	张进江, 郑剑磊, 王海滨, 郭磊, 刘江, 戚国伟. 内蒙古大青山-盘羊山晚中生代-早新生代构造事件及其对华北北缘构造演化的启示[J]. 地学前缘, 2024, 31(1): 127-141.
[4]	万渝生, 董春艳, 颉颃强, 李鹏川, 刘守偈, 李源, 王宇晴, 王堃力, 刘敦一. 华北克拉通新太古代晚期岩浆作用:对构造体制和克拉通化的启示[J]. 地学前缘, 2024, 31(1): 77-94.
[5]	魏春景, 赵亚男, 初航. 冀北红旗营杂岩多期变质作用:古元古代俯冲/碰撞—晚古生代伸展—早中生代挤压的记录[J]. 地学前缘, 2024, 31(1): 95-110.
[6]	杨立强, 和文言, 高雪, 王偲瑞, 李楠, 邱昆峰, 张良, 马强, 苏玉平, 李大鹏, 张智宇, 于红. 克拉通岩石圈三维物质架构示踪方法[J]. 地学前缘, 2023, 30(6): 391-405.
[7]	叶涛, 牛成民, 王德英, 王清斌, 代黎明, 陈安清. 渤海西南海域中生代构造演化、动力学机制及其对华北克拉通破坏的启示[J]. 地学前缘, 2022, 29(5): 133-146.
[8]	万渝生, 董春艳, 李鹏川, 苗培森, 王惠初, 李建荣. 五台地区高凡群形成时代新证据:锆石SHRIMP U-Pb定年[J]. 地学前缘, 2022, 29(2): 45-55.
[9]	刘劲鸿. 吉林蛟河上地幔岩碎块内熔融微区矿物学及其地质意义[J]. 地学前缘, 2020, 27(5): 48-60.
[10]	邵济安, 周新华, 张履桥. 华北克拉通北缘显生宙四次底侵作用及其构造-岩浆活动与深部背景[J]. 地学前缘, 2020, 27(4): 124-134.
[11]	彭润民, 王建平. 华北克拉通北缘西段新元古代裂谷的确认与成矿[J]. 地学前缘, 2020, 27(2): 420-441.
[12]	王盟，钱加慧，张进江，张波. 龙泉关剪切带眼球状花岗质片麻岩锆石U-Pb年代学和Lu-Hf同位素特征及其地质意义[J]. 地学前缘, 2019, 26(3): 171-182.
[13]	刘典波，王小琳，张恒，石成龙. 华北串岭沟组凝灰岩锆石SHRIMP年龄及其地层学意义[J]. 地学前缘, 2019, 26(3): 183-189.
[14]	赵远方, 胡健民, 公王斌, 陈虹. 华北克拉通中部带中段古元古代构造格架与主要变形事件研究 [J]. 地学前缘, 2019, 26(2): 104-119.
[15]	陈威宇，陈衍景，李秋根，李建荣，李凯月，疏孙平，陈西，佟子达. 山西五台山滹沱群四集庄冰碛岩碎屑锆石年龄及其对大氧化事件研究意义[J]. 地学前缘, 2018, 25(5): 1-18.