大兴安岭北段富克山岩浆弧的组成:对蒙古—鄂霍茨克洋南向俯冲的制约

doi:10.13745/j.esf.sf.2021.7.14

摘要/Abstract

摘要：

富克山岩浆弧呈北东向分布于大兴安岭北段富克山—古莲河一带,其物质组成、形成时代及其空间展布规律对于研究蒙古—鄂霍茨克洋晚三叠世地质构造演化具有重要意义。本文对其内的辉长岩、闪长岩、花岗闪长岩进行了岩石学、地球化学及锆石U-Pb定年分析研究,探讨大兴安岭北段晚三叠世时期的构造背景。LA-ICP-MS锆石U-Pb定年获得辉长岩、花岗闪长岩的结晶年龄分别为(205.7±2.2) Ma、(203.2±2.5) Ma,反映了晚三叠世的构造岩浆事件。岩石学和地球化学研究表明,辉长岩、闪长岩具有富钠、高铝、高钙、高镁、高Mg^#值、低钛等特征,属于拉斑系列与钙碱性过渡系列岩石,无明显的Eu负异常,相对富集LILE和LREE,亏损HFSE。花岗闪长岩具有高硅、富钠、高铝、低镁等特征,属于钙碱性系列岩石,高Sr,低Y、Yb,无明显的Eu负异常,显示了O型埃达克质岩石的地球化学特征。富克山岩浆弧的空间展布,具有由北向南的分布规律,指示了蒙古—鄂霍茨克洋具有往南的俯冲极性。

关键词: 大兴安岭北段, 富克山岩浆弧, 晚三叠世, 蒙古—鄂霍茨克洋, 南向俯冲

Abstract:

The Fukeshan magmatic arc extends north-east in Fukeshan-Gulianhe area, northern Great Xing’an Range. Its material composition, formation age and spatial distribution pattern are very important for studying the Late Triassic tectonic evolution of the Mongol-Okhotsk ocean. In this paper, the petrology, geochemistry and zircon U-Pb dating of gabbro, diorite and granodiorite from the Fukeshan magmatic arc are reported, aiming to furthering our understanding of the tectonic setting of the northern Great Xing’an Range during the Late Triassic. LA-ICP-MS zircon U-Pb dating yielded the crystallization ages of (205.7±2.2) Ma and (203.2±2.5) Ma for gabbro and granodiorite, respectively, which correspond to the tectonic-magmatic event in the Late Triassic. Petrological and geochemical study indicate that the gabbro and diorite belong to tholeiite and calc-alkaline transition series rocks with high Na, Al, Ca, Mg and Mg^# contents and low Ti contents. They are enriched in large ion lithophile elements (LIFE) and light rare earth elements (LREE). The granodiorite belongs to calc-alkaline transition series rocks with high Si, Na and Al contents and low Mg contents. The rock has low content of Y and Yb, with no obvious negative Eu anomaly and belongs to O-type adakite. The Fukeshan magmatic arc has a distribution pattern from north to south, and the corresponding lithologic variation indicates the Mongol-Okhotsk ocean has a polarity of southward subduction.

Key words: northern Great Xing’an Range, Fukeshan magmatic arc, Late Triassic, Mongol-Okhotsk ocean, southward subduction

中图分类号:

P581
P597

李文龙, 杨晓平, 钱程, 李成禄, 吕明奇, 程招勋, 王立佳. 大兴安岭北段富克山岩浆弧的组成:对蒙古—鄂霍茨克洋南向俯冲的制约[J]. 地学前缘, 2022, 29(2): 146-163.

LI Wenlong, YANG Xiaoping, QIAN Cheng, LI Chenglu, LÜ Mingqi, CHENG Zhaoxun, WANG Lijia. Composition of the Fukeshan magmatic arc in the northern Great Xing’an Range: Constraints on the southward subduction of the Mongol-Okhotsk oceanic plate[J]. Earth Science Frontiers, 2022, 29(2): 146-163.

图/表 13

图1 富克山地区地质简图 (a据文献[1]修改,b据文献[2]修改)

Fig.1 Geological sketch maps of the Fukeshan area. a modified after [1]; b modified after [2].

图2 富克山地区侵入岩典型岩石露头及显微照片 a—早侏罗世正长花岗岩中的闪长岩捕虏体;b—晚三叠世花岗闪长岩中的寒武纪片麻状花岗岩捕虏体;c—晚三叠世花岗闪长岩中的镁铁质包体;d—辉长岩野外露头;e—闪长岩野外露头,被早侏罗世正长花岗岩侵入;f—花岗闪长岩野外露头;g—辉长岩镜下照片;h—闪长岩镜下照片;i—花岗闪长岩镜下照片。Pl—斜长石;Px—辉石;Hb—角闪石;Bi—黑云母;Q—石英。

Fig.2 Typical field rock outcrops and photomicrographs of Late Triassic intrusive rocks of Fukeshan area

图3 富克山地区晚三叠世辉长岩锆石阴极发光(CL)图像(PM4LT2)

Fig.3 Cathodeluminescence (CL) images of analyzed zircon (PM4LT2) from Late Triassic gabbro of Fukeshan area

表1 富克山地区晚三叠世辉长岩锆石U-Pb测年数据及年龄(PM4LT2)

Table 1 Zircon U-Pb data and age (PM4LT2) of Late Triassic gabbro in Fukeshan area

表2 英云闪长岩及闪长岩主量元素、微量元素分析结果及参数

Table 2 Major and trace element contents of the tonalite and the diorite

图4 富克山地区晚三叠世侵入岩锆石U-Pb年龄谐和图

Fig.4 U-Pb concordia diagrams for volcanic rocks from Late Triassic intrusive rocks of Fukeshan area

图5 富克山地区晚三叠世花岗闪长岩锆石阴极发光(CL)图像(PM12LT56)

Fig.5 Cathodeluminescence (CL) images of analyzed zircon (PM12LT56) from Late Triassic granodiorite of Fukeshan area

表3 富克山地区晚三叠世侵入岩主微量元素及稀土元素分析结果

Table 3 Major element, trace element and rare element compositions of Late Triassic intrusive rocks of Fukeshan area

图6 富克山地区晚三叠世侵入岩主量元素图解 (a-d分别据文献[39,40,41,42]修改)

Fig.6 Major element diagrams for volcanic rocks from Late Triassic intrusive rocks of Fukeshan area. Modified after [39-42].

图7 富克山地区晚三叠世侵入岩球粒陨石标准化稀土元素配分模式图(a)和原始地幔标准化微量元素蛛网图(b) (球粒陨石数值引自文献[43], 原始地幔数值引自文献[44])

Fig.7 (a) Chondrite-normalized rare earth element patterns (data from [43]) and (b) primitive mantle-normalized trace element spider diagrams (data from [44]) for Late Triassic intrusive rocks of Fukeshan area

图8 富克山地区晚三叠世侵入岩La/Sm-Ba/Th(a)、Ba/La-Th/Yb(b)判别图解 (据文献[60]修改)

Fig.8 La/Sm-Ba/Th (a) and Ba/La-Th/Yb (b) diagrams for Late Triassic intrusive rocks of Fukeshan area. Modified after 60.

图9 富克山地区晚三叠世侵入岩Sm/Yb-Sm(a)、La/Yb-Zr/Nb(b)判别图解 (a据文献[61,62,63]修改,b据文献[64]修改) DM—亏损地幔;PM—原始地幔:N-MORB—正常大洋中脊玄武岩;MORB—洋中脊玄武岩;OIB—洋岛玄武岩。

Fig.9 (a) Sm/Yb-Sm (modified after [61-63]) and (b) La/Yb-Zr/Nb (modified after [64]) diagrams for Late Triassic intrusive rocks of Fukeshan area

图10 富克山地区晚三叠世侵入岩Y-Sr/Y(a)、YbN-(La/Yb)N(b)判别图解 (a据文献[77]修改;b据文献[78]修改)

Fig.10 (a) Sr/Y-Y (modified after [77]) and (b) (La/Yb)N-YbN (modified after [78]) for Late-Triassic intrusive rocks of Fukeshan area

参考文献 92

[1]	ZHOU J B, WILDE S A, ZHAO G C, et al. Pan-African metamorphic and magmatic rocks of the Khanka Massif, NE China: further evidence regarding their affinity[J]. Geological Magazine, 2010, 147(5):737-749. DOI URL
[2]	ZHOU J B, HAN J, ZHAO G C, et al. The emplacement time of the Hegenshan ophiolite: constraints from the unconformably overlying Paleozoic strata[J]. Tectonophysics, 2015, 662:398-415. DOI URL
[3]	MENG E, XU W L, PEI F P, et al. Detrital-zircon geochronology of Late Paleozoic sedimentary rocks in eastern Heilongjiang Province, NE China: implications for the tectonic evolution of the eastern segment of the Central Asian Orogenic Belt[J]. Tectonophysics, 2010, 485(1/2/3/4):42-51. DOI URL
[4]	WANG F, XU W L, MENG E, et al. Early Paleozoic amalgamation of the Songnen-Zhangguangcai Range and Jiamusi massifs in the eastern segment of the Central Asian Orogenic Belt: geochronological and geochemical evidence from granitoids and rhyolites[J]. Journal of Asian Earth Sciences, 2012, 49:234-248. DOI URL
[5]	冯志强, 刘永江, 金巍, 等. 东北大兴安岭北段蛇绿岩的时空分布及与区域构造演化关系的研究[J]. 地学前缘, 2019, 26(2):120-136.
[6]	LI Y, XU W L, WANG F, et al. Geochronology and geochemistry of Late Paleozoic volcanic rocks on the western margin of the Songnen-Zhangguangcai Range Massif, NE China: implications for the amalgamation history of the Xing’an and Songnen-Zhangguangcai Range massifs[J]. Lithos, 2014, 205:394-410. DOI URL
[7]	GE W C, CHEN J S, YANG H, et al. Tectonic implications of new zircon U-Pb ages for the Xinghuadukou Complex, Erguna Massif, northern Great Xing’an Range, NE China[J]. Journal of Asian Earth Sciences, 2015, 106:169-185. DOI URL
[8]	王成文, 金巍, 张兴洲, 等. 东北及邻区晚古生代大地构造属性新认识[J]. 地层学杂志, 2008, 32(2):119-136.
[9]	刘永江, 张兴洲, 金巍, 等. 东北地区晚古生代区域构造演化[J]. 中国地质, 2010, 37(4):943-951.
[10]	LIU Y J, LI W M, FENG Z Q, et al. A review of the Paleozoic tectonics in the eastern part of Central Asian Orogenic Belt[J]. Gondwana Research, 2017, 43:123-148. DOI URL
[11]	许文良, 王枫, 裴福萍, 等. 中国东北中生代构造体制与区域成矿背景: 来自中生代火山岩组合时空变化的制约[J]. 岩石学报, 2013, 29(2):339-353.
[12]	徐备, 赵盼, 鲍庆中, 等. 兴蒙造山带前中生代构造单元划分初探[J]. 岩石学报, 2014, 30(7):1841-1857.
[13]	李锦轶, 刘建峰, 曲军峰, 等. 中国东北地区古生代构造单元: 地块还是造山带?[J]. 地球科学, 2019, 44(10):3157-3177.
[14]	李锦轶, 刘建峰, 曲军峰, 等. 中国东北地区主要地质特征和地壳构造格架[J]. 岩石学报, 2019, 35(10):2989-3016.
[15]	KRAVCHINSKY V A, COGNÉ J P, HARBERT W P, et al. Evolution of the Mongol-Okhotsk Ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk suture zone, Siberia[J]. Geophysical Journal International, 2002, 148(1):34-57. DOI URL
[16]	COGNÉ J P, KRAVCHINSKY V A, HALIM N, et al. Late Jurassic-Early Cretaceous closure of the Mongol-Okhotsk ocean demonstrated by new Mesozoic palaeomagnetic results from the Trans-Baïkal area (SE Siberia)[J]. Geophysical Journal International, 2005, 163(2):813-832. DOI URL
[17]	KELTY T K, YIN A, DASH B, et al. Detrital-zircon geochronology of Paleozoic sedimentary rocks in the Hangay-Hentey Basin, North-central Mongolia: implications for the tectonic evolution of the Mongol-Okhotsk Ocean in Central Asia[J]. Tectonophysics, 2008, 451(1/2/3/4):290-311. DOI URL
[18]	唐杰, 许文良, 王枫, 等. 额尔古纳地块J₃-K₁岩浆作用及其变形历史: 对蒙古—鄂霍茨克缝合带晚中生代构造演化的制约[C]// 中国矿物岩石地球化学学会第十五届学术年会论文集. 长沙: 中国矿物岩石地球化学学会, 2015.
[19]	DONSKAYA T V, GLADKOCHUB D P, MAZUKABZOV A M, et al. Late Paleozoic-Mesozoic subduction related magmatism at the southern margin of the Siberian continent and the 150 million-year history of the Mongol-Okhotsk ocean[J]. Journal of Asian Earth Sciences, 2013, 62:79-97. DOI URL
[20]	王伟, 许文良, 王枫, 等. 满洲里—额尔古纳地区中生代花岗岩的锆石U-Pb年代学与岩石组合: 对区域构造演化的制约[J]. 高校地质学报, 2012, 18(1):88-105.
[21]	TANG J, XU W L, WANG F, et al. Geochronology and geochemistry of Early-Middle Triassic magmatism in the Erguna Massif, NE China: constraints on the tectonic evolution of the Mongol-Okhotsk ocean[J]. Lithos, 2014,184/185/186/187:1-16.
[22]	WU F Y, SUN D Y, GE W C, et al. Geochronology of the Phanerozoic granitoids in northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41(1):1-30. DOI URL
[23]	赵硕, 许文良, 王枫, 等. 额尔古纳地块新元古代岩浆作用: 锆石U-Pb年代学证据[J]. 大地构造与成矿学, 2016, 40(3):559-573.
[24]	SUN D Y, GOU J, WANG T H, et al. Geochronological and geochemical constraints on the Erguna Massif basement, NE China-subduction history of the Mongol-Okhotsk oceanic crust[J]. International Geology Review, 2013, 55(14):1801-1816. DOI URL
[25]	TANG J, XU W L, WANG F, et al. Early Mesozoic southward subduction history of the Mongol-Okhotsk oceanic plate: evidence from geochronology and geochemistry of Early Mesozoic intrusive rocks in the Erguna Massif, NE China[J]. Gondwana Research, 2016, 31:218-240. DOI URL
[26]	李良, 孙丰月, 李碧乐, 等. 漠河地区黑云母花岗闪长岩地球化学、Hf同位素特征及其成因[J]. 地球科学, 2018, 43(2):417-435.
[27]	李强, 程学芹, 陈伟, 等. 额尔古纳地块早—中三叠世安山岩的发现及其对蒙古—鄂霍茨克洋南向俯冲的指示[J]. 地球科学, 2021, 46(8):2768-2785.
[28]	GOU J, SUN D Y, REN Y S, et al. Geochemical and Hf isotopic compositions of Late Triassic-Early Jurassic intrusions of the Erguna Block, Northeast China: petrogenesis and tectonic implications[J]. International Geology Review, 2017, 59(3):347-367. DOI URL
[29]	付俊彧, 那福超, 李仰春, 等. 蒙古—鄂霍茨克洋南向俯冲:小兴安岭西北部“落马湖群”中三叠世岩浆记录[J]. 地质通报, 2021, 40(6):889-904.
[30]	李锦轶. 中国东北及邻区若干地质构造问题的新认识[J]. 地质论评, 1998, 44(4):339-347.
[31]	张兴洲, 周建波, 迟效国, 等. 东北地区晚古生代构造-沉积特征与油气资源[J]. 吉林大学学报(地球科学版), 2008, 38(5):719-725.
[32]	张兴洲, 马玉霞, 迟效国, 等. 东北及内蒙古东部地区显生宙构造演化的有关问题[J]. 吉林大学学报(地球科学版), 2012, 42(5):1269-1285.
[33]	ZHOU J B, WILDE S A, ZHANG X Z, et al. Early Paleozoic metamorphic rocks of the Erguna block in the Great Xing’an Range, NE China: evidence for the timing of magmatic and metamorphic events and their tectonic implications[J]. Tectonophysics, 2011, 499(1/2/3/4):105-117. DOI URL
[34]	WU G, CHEN Y C, CHEN Y J, et al. Zircon U-Pb ages of the metamorphic supracrustal rocks of the Xinghuadukou Group and granitic complexes in the Argun Massif of the northern Great Hinggan Range, NE China, and their tectonic implications[J]. Journal of Asian Earth Sciences, 2012, 49:214-233. DOI URL
[35]	赵硕, 许文良, 唐杰, 等. 额尔古纳地块“新元古代”佳疙瘩组的形成时代: 来自锆石U-Pb年代学的制约[C]// 中国矿物岩石地球化学学会第15届学术年会论文摘要集. 长春: 中国矿物岩石地球化学学会, 2015.
[36]	ZHANG Y H, XU W L, TANG J, et al. Age and provenance of the Ergunahe Group and the Wubinaobao Formation, northeastern Inner Mongolia, NE China: implications for tectonic setting of the Erguna Massif[J]. International Geology Review, 2014, 56(6):653-671. DOI URL
[37]	李怀坤, 耿建珍, 郝爽, 等. 用激光烧蚀多接收器等离子体质谱仪(LA-MC-ICPMS)测定锆石U-Pb同位素年龄的研究[J]. 矿物学报, 2009, 29(S1):600-601.
[38]	RAPP R P. Amphibole-out phase boundary in partially melted metabasalt, its control over liquid fraction and composition, and source permeability[J]. Journal of Geophysical Research: Solid Earth, 1995, 100(B8):15601-15610.
[39]	MIDDLEMOST E A K. Naming materials in the magma/igneous rock system[J]. Earth-Science Reviews, 1994, 37(3/4):215-224. DOI URL
[40]	PECCERILLO A, TAYLOR S R. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976, 58(1):63-81. DOI URL
[41]	MIYASHIRO A. Volcanic rock series in island arcs and active continental margins[J]. American Journal of Science, 1974, 274(4):321-355. DOI URL
[42]	肖庆辉, 邓晋福, 马达栓, 等. 花岗岩研究思维与方法[M]. 北京: 地质出版社, 2002.
[43]	BOYNTON W V. Cosmochemistry of the rare earth elements: Meteorite studies[M]// Rare Earth Element Geochemistry. Amsterdam: Elsevier, 1984: 63-114.
[44]	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
[45]	ZHANG L C, ZHOU X H, YING J F, et al. Geochemistry and Sr-Nd-Pb-Hf isotopes of Early Cretaceous basalts from the Great Xinggan Range, NE China: implications for their origin and mantle source characteristics[J]. Chemical Geology, 2008, 256(1/2):12-23. DOI URL
[46]	YING J F, ZHOU X H, ZHANG L C, et al. Geochronological framework of Mesozoic volcanic rocks in the Great Xing’an Range, NE China, and their geodynamic implications[J]. Journal of Asian Earth Sciences, 2010, 39(6):786-793. DOI URL
[47]	孟恩, 许文良, 杨德彬, 等. 满洲里地区灵泉盆地中生代火山岩的锆石U-Pb年代学、地球化学及其地质意义[J]. 岩石学报, 2011, 27(4):1209-1226.
[48]	YU J J, WANG F, XU W L, et al. Early Jurassic mafic magmatism in the Lesser Xing’an-Zhangguangcai Range, NE China, and its tectonic implications: constraints from zircon U-Pb chronology and geochemistry[J]. Lithos, 2012, 142/143:256-266. DOI URL
[49]	GUO P, XU W L, YU J J, et al. Geochronology and geochemistry of Late Triassic bimodal igneous rocks at the eastern margin of the Songnen-Zhangguangcai Range Massif, Northeast China: petrogenesis and tectonic implications[J]. International Geology Review, 2016, 58(2):196-215. DOI URL
[50]	YANG H, GE W C, ZHAO G C, et al. Late Triassic intrusive complex in the Jidong region, Jiamusi-Khanka Block, NE China: geochemistry, zircon U-Pb ages, Lu-Hf isotopes, and implications for magma mingling and mixing[J]. Lithos, 2015, 224/225:143-159. DOI URL
[51]	WANG F, XU W L, XU Y G, et al. Late Triassic bimodal igneous rocks in eastern Heilongjiang Province, NE China: implications for the initiation of subduction of the Paleo-Pacific Plate beneath Eurasia[J]. Journal of Asian Earth Sciences, 2015, 97:406-423. DOI URL
[52]	周长勇, 吴福元, 葛文春, 等. 大兴安岭北部塔河堆晶辉长岩体的形成时代、地球化学特征及其成因[J]. 岩石学报, 2005, 21(3):763-775.
[53]	赵芝, 迟效国, 刘建峰, 等. 内蒙古牙克石地区晚古生代弧岩浆岩: 年代学及地球化学证据[J]. 岩石学报, 2010, 26(11):3245-3258.
[54]	FENG Z Q, JIA J, LIU Y J, et al. Geochronology and geochemistry of the carboniferous magmatism in the northern Great Xing’an Range, NE China: constraints on the timing of amalgamation of Xing’an and Songnen Blocks[J]. Journal of Asian Earth Sciences, 2015, 113:411-426. DOI URL
[55]	LIU Q, ZHAO G C, HAN Y G, et al. Timing of the final closure of the Paleo-Asian ocean in the Alxa Terrane: constraints from geochronology and geochemistry of Late Carboniferous to Permian gabbros and diorites[J]. Lithos, 2017, 274/275:19-30. DOI URL
[56]	ZHENG Y F, CHEN Y X, DAI L Q, et al. Developing plate tectonics theory from oceanic subduction zones to collisional orogens[J]. Science China: Earth Sciences, 2015, 58(7):1045-1069. DOI URL
[57]	WANG H, WU Y B, QIN Z W, et al. Age and geochemistry of Silurian gabbroic rocks in the Tongbai orogen, Central China: implications for the geodynamic evolution of the North Qinling arc-back-arc system[J]. Lithos, 2013, 179:1-15. DOI URL
[58]	THOMPSON R N, MORRISON M A. Asthenospheric and lower-lithospheric mantle contributions to continental extensional magmatism: an example from the British Tertiary Province[J]. Chemical Geology, 1988, 68(1/2):1-15. DOI URL
[59]	SMITH E I, SÁNCHEZ A, WALKER J D, et al. Geochemistry of mafic magmas in the Hurricane volcanic field, Utah: implications for small- and large-scale chemical variability of the lithospheric mantle[J]. Journal of Geology, 1999, 107(4):433-448. DOI URL
[60]	TATSUMI Y. High-Mg andesites in the Setouchi volcanic belt, southwestern Japan: analogy to Archean magmatism and continental crust formation?[J]. Annual Review of Earth and Planetary Sciences, 2006, 34(1):467-499. DOI URL
[61]	ALDANMAZ E, PEARCE J A, THIRLWALL M F, et al. Petrogenetic evolution of Late Cenozoic, post-collision volcanism in western Anatolia, Turkey[J]. Journal of Volcanology and Geothermal Research, 2000, 102(1/2):67-95. DOI URL
[62]	ZHAO J H, ZHOU M F. Geochemistry of Neoproterozoic mafic intrusions in the Panzhihua district (Sichuan Province, SW China): implications for subduction-related metasomatism in the upper mantle[J]. Precambrian Research, 2007, 152(1/2):27-47. DOI URL
[63]	ZHAO J H, ZHOU M F. Secular evolution of the Neoproterozoic lithospheric mantle underneath the northern margin of the Yangtze Block, South China[J]. Lithos, 2009, 107(3/4):152-168. DOI URL
[64]	ALDANMAZ E, KÖPRÜBAŞI N, GÜRER Ö F, et al. Geochemical constraints on the Cenozoic, OIB-type alkaline volcanic rocks of NW Turkey: implications for mantle sources and melting processes[J]. Lithos, 2006, 86(1/2):50-76. DOI URL
[65]	JAHN B M, WU F Y, CHEN B. Massive granitoid generation in Central Asia: Nd isotope evidence and implication for continental growth in the Phanerozoic[J]. Episodes, 2000, 23(2):82-92. DOI URL
[66]	葛文春, 吴福元, 周长勇, 等. 大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约[J]. 科学通报, 2005, 50(12):1239-1247.
[67]	CAO H H, XU W L, PEI F P, et al. Zircon U-Pb geochronology and petrogenesis of the Late Paleozoic-Early Mesozoic intrusive rocks in the eastern segment of the northern margin of the North China Block[J]. Lithos, 2013, 170/171:191-207. DOI URL
[68]	葛文春, 隋振民, 吴福元, 等. 大兴安岭东北部早古生代花岗岩锆石U-Pb年龄、Hf同位素特征及地质意义[J]. 岩石学报, 2007, 23(2):423-440.
[69]	孙立新, 任邦方, 赵凤清, 等. 内蒙古额尔古纳地块古元古代末期的岩浆记录: 来自花岗片麻岩的锆石U-Pb年龄证据[J]. 地质通报, 2013, 32(Z1):341-352.
[70]	林强, 葛文春, 吴福元, 等. 大兴安岭中生代花岗岩类的地球化学[J]. 岩石学报, 2004, 20(3):403-412.
[71]	董增产, 辜平阳, 陈锐明, 等. 柴北缘西端盐场北山二长花岗岩年代学、地球化学及其Hf同位素特征[J]. 地球科学: 中国地质大学学报, 2015, 40(1):130-144.
[72]	DEFANT M J, DRUMMOND M S. Derivation of some modern arc magmas by melting of young subducted lithosphere[J]. Nature, 1990, 347(6294):662-665. DOI URL
[73]	张旗, 许继峰, 王焰, 等. 埃达克岩的多样性[J]. 地质通报, 2004, 23(Z2):959-965.
[74]	ARCULUS R J. Aspects of magma genesis in arcs[J]. Lithos, 1994, 33(1/2/3):189-208. DOI URL
[75]	RAPP R P, SHIMIZU N, NORMAN M D, et al. Reaction between slab-derived melts and peridotite in the mantle wedge: experimental constraints at 3.8 GPa[J]. Chemical Geology, 1999, 160(4):335-356. DOI URL
[76]	董申保, 田伟. 埃达克岩的原义、特征与成因[J]. 地学前缘, 2004, 11(4):585-594.
[77]	CASTILLO P R. Adakite petrogenesis[J]. Lithos, 2012,134/135:304-316.
[78]	DEFANT M J, DRUMMOND M S. Derivation of some modern arc magmas by melting of young subducted lithosphere[J]. Nature, 1990, 347(6294):662-665. DOI URL
[79]	LIU H C, LI Y L, HE H Y, et al. Two-phase southward subduction of the Mongol-Okhotsk oceanic plate constrained by Permian-Jurassic granitoids in the Erguna and Xing’an massifs (NE China)[J]. Lithos, 2018,304/305/306/307:347-361.
[80]	LI Y, XU W L, TANG J, et al. Geochronology and geochemistry of Mesozoic intrusive rocks in the Xing’an Massif of NE China: implications for the evolution and spatial extent of the Mongol-Okhotsk tectonic regime[J]. Lithos, 2018,304/305/306/307:57-73.
[81]	陈志广, 张连昌, 卢百志, 等. 内蒙古太平川铜钼矿成矿斑岩时代、地球化学及地质意义[J]. 岩石学报, 2010, 26(5):1437-1449.
[82]	OUYANG H G, MAO J W, SANTOSH M, et al. Geodynamic setting of Mesozoic magmatism in NE China and surrounding regions: perspectives from spatio-temporal distribution patterns of ore deposits[J]. Journal of Asian Earth Sciences, 2013, 78:222-236. DOI URL
[83]	李春风, 柳振江, 宓奎峰, 等. 内蒙古八大关斑岩型铜钼矿床形成时代与成因分析[J]. 中国地质, 2014, 41(4):1253-1269.
[84]	WANG W, TANG J, XU W L, et al. Geochronology and geochemistry of Early Jurassic volcanic rocks in the Erguna Massif, Northeast China: petrogenesis and implications for the tectonic evolution of the Mongol-Okhotsk suture belt[J]. Lithos, 2015, 218/219:73-86. DOI URL
[85]	YANG H, GE W C, YU Q, et al. Zircon U-Pb-Hf isotopes, bulk-rock geochemistry and petrogenesis of Middle to Late Triassic I-type granitoids in the Xing’an Block, Northeast China: implications for Early Mesozoic tectonic evolution of the Central Great Xing’an Range[J]. Journal of Asian Earth Sciences, 2016, 119:30-48. DOI URL
[86]	马永非, 刘永江, 温泉波, 等. 大兴安岭中段晚三叠世哈达陶勒盖组火山岩成因及构造背景[J]. 地球科学, 2017, 42(12):2146-2173.
[87]	赵院冬, 车继英, 吴大天, 等. 小兴安岭西北部早—中侏罗世TTG花岗岩年代学、地球化学特征及构造意义[J]. 吉林大学学报(地球科学版), 2017, 47(4):1119-1137.
[88]	李宇, 丁磊磊, 许文良, 等. 孙吴地区中侏罗世白云母花岗岩的年代学与地球化学: 对蒙古—鄂霍茨克洋闭合时间的限定[J]. 岩石学报, 2015, 31(1):56-66.
[89]	赵院冬, 车继英, 许逢明, 等. 兴安地块东北部晚侏罗世C型埃达克质花岗岩年代学、地球化学特征及构造环境意义[J]. 地学前缘, 2018, 25(6):240-253.
[90]	钱程, 汪岩, 陆露, 等. 大兴安岭北段扎兰屯地区斜长角闪岩年代学、地球化学和Hf同位素特征及其构造意义[J]. 地球科学, 2019, 44(10):3193-3208.
[91]	李锦轶, 张进, 刘建峰, 等. 中国大陆主要变形系统[J]. 地学前缘, 2014, 21(3):226-245.
[92]	邓晋福, 冯艳芳, 狄永军, 等. 岩浆弧火成岩构造组合与洋陆转换[J]. 地质论评, 2015, 61(3):473-484.