松辽盆地白垩纪综合年代地层格架

doi:10.13745/j.esf.sf.2024.1.22

地学前缘 ›› 2024, Vol. 31 ›› Issue (1): 431-445.DOI: 10.13745/j.esf.sf.2024.1.22

• 环境变化与生物圈层相互作用 • 上一篇下一篇

松辽盆地白垩纪综合年代地层格架

吴怀春¹^,²^,³(), 李山¹^,²^,³, 王成善¹^,³^,⁴, 褚润健¹^,³^,⁴, 王璞珺⁵, 高远¹^,³^,⁴, 万晓樵¹^,⁴, 贺怀宇⁶, 邓成龙⁶, 杨光⁷, 黄永建¹^,⁴, 高有峰⁵, 席党鹏¹^,⁴, 王天天¹^,³, 房强¹^,²^,³, 杨天水¹^,³^,⁴, 张世红¹^,³^,⁴

1.中国地质大学(北京) 生物地质与环境地质国家重点实验室, 北京 100083
2.中国地质大学(北京) 海洋学院, 北京 100083
3.中国地质大学(北京) 深时数字地球前沿科学中心, 北京 100083
4.中国地质大学(北京) 地球科学与资源学院, 北京 100083
5.吉林大学地球科学学院, 吉林长春 130061
6.中国科学院地质与地球物理研究所岩石圈演化国家重点实验室, 北京 100029
7.中国石油吉林油田分公司勘探部, 吉林松原 138000

收稿日期:2023-12-12 修回日期:2024-01-05 出版日期:2024-01-25 发布日期:2024-01-25
作者简介:吴怀春(1977—),男,教授,主要从事海洋地质学、旋回地层学和古地磁学的教学和科研工作。E-mail: whcgeo@cugb.edu.cn
基金资助:
国家自然科学基金项目(41925010);国家自然科学基金项目(41790451);教育部、科学技术部高等学校学科创新引智计划(“111计划”)项目(B20011)

Integrated chronostratigraphic framework for Cretaceous strata in the Songliao Basin

WU Huaichun¹^,²^,³(), LI Shan¹^,²^,³, WANG Chengshan¹^,³^,⁴, CHU Runjian¹^,³^,⁴, WANG Pujun⁵, GAO Yuan¹^,³^,⁴, WAN Xiaoqiao¹^,⁴, HE Huaiyu⁶, DENG Chenglong⁶, YANG Guang⁷, HUANG Yongjian¹^,⁴, GAO Youfeng⁵, XI Dangpeng¹^,⁴, WANG Tiantian¹^,³, FANG Qiang¹^,²^,³, YANG Tianshui¹^,³^,⁴, ZHANG Shihong¹^,³^,⁴

1. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (Beijing), Beijing 100083, China
2. School of Ocean Sciences, China University of Geosciences (Beijing), Beijing 100083, China
3. Frontiers Science Center for Deep-time Digital Earth, China University of Geosciences (Beijing), Beijing 100083, China
4. School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, China
5. College of Earth Sciences, Jilin University, Changchun 130061, China
6. Stale Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
7. Exploration Department, Jilin Oilfield Company, PetroChina, Songyuan 138000, China

Received:2023-12-12 Revised:2024-01-05 Online:2024-01-25 Published:2024-01-25

摘要/Abstract

摘要：

白垩纪是典型的温室气候时期,也是全球大规模烃源岩形成时期,但对于温室气候背景下陆地的环境状态、气候变化、生命响应及其演化规律尚不清楚;陆相有机质及大规模烃源岩堆积与气候环境变化之间的关系还不明确。中国东北的松辽盆地发育了世界上最完整的白垩纪陆相沉积记录,烃源岩在盆地内广泛分布,是研究白垩纪陆地气候-环境变化和烃源岩形成机制的绝佳地点。但由于露头剖面沉积记录“连续性”和“完整性”较差,缺乏高精度的综合年代地层格架约束,导致松辽盆地的地层划分与对比存在较多争议,一定程度上阻碍了白垩纪陆地古气候、古环境演化的研究进程。松辽盆地国际大陆科学钻探计划实施的松科1井、松科2井和松科3井共钻取了8 197 m完整且连续的白垩纪陆相地层岩心记录。本文通过综合科探井岩石地层学、生物地层学、磁性地层学、同位素年代学和旋回地层学的研究成果,建立了松辽盆地白垩纪高分辨率综合年代地层格架,为探索白垩纪陆地深时气候-环境演化及服务松辽盆地油气勘探可持续发展提供了精细的年代学证据。

关键词: 白垩纪, 国际大陆科学钻探项目(ICDP), 松辽盆地, 地质年代学, 旋回地层学

Abstract:

The Cretaceous is a typical greenhouse period with global large scale formation of organic-rich source rocks. However, we have only limited understanding of the terrestrial environmental status, climate change and biosphere responses and evolution during the greenhouse period; the effect of climate and environmental changes on the terrestrial organic accumulation and large scale source rock formation remains unclear. To study these issues the Songliao Basin in northeastern China offers an unique opportunity. The Songliao Basin has widespread distribution of Cretaceous source rocks and possesses the most complete sedimentary record of the Cretaceous in the world. One challenges, however, was the lack of high-quality rock records due to low continuity and low completeness of the records, which has caused controversies over the stratigraphic division of the Songliao Basin. Recently, the 8197 m drill core obtained from ICDP (Continental Scientific Drilling Program) boreholes (SK-1, SK-2, SK-3) provided a virtually complete terrestrial stratigraphic record of Cretaceous strata of the basin. In this study, by evidence synthesis using results of lithostratigraphy, biostratigraphy, magnetostratigraphy, radioisotope geochronology, and cyclostratigraphy, we constructed a high-resolution, integrated Cretaceous chronostratigraphic framework for the Songliao Basin, which provided fine chronological reference for studying the evolution of deep-time Cretaceous climate and environment as well as promoting sustainable oil and gas development in the Songliao Basin.

Key words: Cretaceous, International Continental Scientific Drilling Program (ICDP), Songliao Basin, geochronology, cyclostratigraphy

中图分类号:

P534.53
P535

吴怀春, 李山, 王成善, 褚润健, 王璞珺, 高远, 万晓樵, 贺怀宇, 邓成龙, 杨光, 黄永建, 高有峰, 席党鹏, 王天天, 房强, 杨天水, 张世红. 松辽盆地白垩纪综合年代地层格架[J]. 地学前缘, 2024, 31(1): 431-445.

WU Huaichun, LI Shan, WANG Chengshan, CHU Runjian, WANG Pujun, GAO Yuan, WAN Xiaoqiao, HE Huaiyu, DENG Chenglong, YANG Guang, HUANG Yongjian, GAO Youfeng, XI Dangpeng, WANG Tiantian, FANG Qiang, YANG Tianshui, ZHANG Shihong. Integrated chronostratigraphic framework for Cretaceous strata in the Songliao Basin[J]. Earth Science Frontiers, 2024, 31(1): 431-445.

图/表 6

图1 松辽盆地地质背景图(据文献[40]修改) a—晚白垩世(约90 Ma)全球古地理图,红星表示松辽盆地位置;b—松辽盆地一级构造单元及松科1井南、北井(SK-1s, SK-1n)、松科2井(SK-2)和松科3井(SK-3)井位分布;c—基于横跨松辽盆地中部的区域地震资料(A-A')的构造截面示意图。

Fig.1 Geological setting of the Songliao Basin. Modified after [40].

图3 松辽盆地火石岭组—明水组沉积环境演化(据文献[21,23]修改)

Fig.3 Evolution of Cretaceous sedimentary environment of the Huoshiling-Mingshui Formations in the Songliao Basin. Modified after [21,23].

图2 松辽盆地白垩纪综合年代地层格架与重大地质事件(据文献[11,39-40,44⇓⇓⇓⇓⇓-50]修改) 地质事件为大洋缺氧事件(oceanic anoxic event, OAE)、湖泊缺氧事件(lake anoxic event, LAE);OAE1d?和OAE2?表示年代学约束下的OAE发生层段[44];红字均为U-Pb CA-ID-TIMS定年结果[45-46];各阶的年龄取自国际年代地层表(2023)[47];天文年代标尺(astronomical time scale, ATS)。

Fig.2 Integrated Cretaceous chronostratigraphic framework for the Songliao Basin, with major geological events indicated. Modified after [11,39-40,44⇓⇓⇓⇓⇓-50].

表1 松科1井上白垩统生物地层格架(据文献[37])

Table 1 Biostratigraphic framework for Upper Cretaceous strata, borehole SK-1. Adapted from [37].

统	组	化石组合
统	组	介形类	孢粉	轮藻
上白垩统	四方台组	Talicypridea amoena-Tumiasevia kaitunensis-Paracandona qiananensis	Ulmipollenites-Ulmoideipites	Atopochara ulanensis
	嫩江组	Cypridea squalida-C.anonyma-C.spiniferusa Cypridea gunsulinensis-C.ardua Cypridea ordinata-Ilyocyprimorpha netchaevae Cypridea spongvosa-Strumosia salebrosa Talicypridea augusta-Harbinia hapla	Aquilapollenites	Songliaochara heilongjiangensis-Charites cretacea
	姚家组	Cypridea exornata-Lycopterocypris retractilis Cypridea dorsoangula-Ziziphocypris concta	Borealipollis	Aclistochara songliaoensis
	青山口组	Triangulicypris torsuosus-T.torsuosus Cypridea dekhoinensis-Limnocypridea copiosa Limnocypridea inflata-Sunliavia tumida Cypridea panda-Triangulicypris fusiformis
	泉头组	Cypridea albidula-C. prognata-Mongolianella palmosa Cypridea ellipitica-Candona curva	Trilobosporites-Cyathidites- Tricolpopollenites Schizaeoisporites- Quantonenpollenites-Tricolporopollenites	Amblyochara quantouensis

表2 松辽盆地科探井白垩纪地层格架

Table 2 Stratigraphic framework for Cretaceous strata in studied boreholes

组	研究钻孔	深度范围/m	年龄范围/Ma	时代划分
明水组	SK-1n	210.7~807.12	65.07~72.86	坎潘期—古近纪丹麦期
四方台组	SK-1n	807.12~1021.6	72.86~76.08	坎潘期
嫩江组	SK-1n	1 021.6~1 796.75	76.08~85.21	圣通期—坎潘期
	SK-1s	960~1 128.17
	SK-2	435.125~1 250.5
姚家组	SK-1s	1 128.17~1 285.91	85.21~86.3	康尼亚克期—圣通期
姚家组	SK-2	1 250.5~1 371	85.21~86.3	康尼亚克期—圣通期
青山口组	SK-1s	1 285.91~1 782.93	86.3~91.82	土伦期—康尼亚克期
	SK-2	1 371~1 676.5
	SK-3	675~757
泉头组	SK-1s	1 782.93~1 915.0	91.82~98.83	塞诺曼期—土伦期
	SK-2	1 676.5~2 535.5
	SK-3	757~1 725
登娄库组	SK-3	1 725~2 400	98.83~102.74	阿尔布期—塞诺曼期
营城组	SK-2	2 969.21~3 335.99	102.74~110.4	阿尔布期
沙河子组	SK-2	3 335.99~5 960	110.4~117.8	阿普特期
火石岭组	SK-2	5 720.4~6 242.4

图4 松辽盆地白垩纪国际大陆科学钻探松科1井、松科2井和松科3井天文年代标尺 a—松科1井北井明水组—四方台组天文年代标尺,a1—时间域频谱分析数据源自Wu等[64];b—松科1井北井嫩江组天文年代标尺,b1—时间域频谱分析数据源自Wu等[64];c—松科1井南井泉头组—嫩江组天文年代标尺,c1—时间域频谱分析数据源自Wu等[40];d—松科2井泉头组—嫩江组天文年代标尺,d1—时间域频谱分析数据源自Ma等[106];e—松科3井登娄库组—青山口组天文年代标尺,e1—时间域频谱分析数据源自Li等[44];f—松科2井沙河子组—嫩江组天文年代标尺,f1—时间域频谱分析数据源自麻晓娟等[105]。

Fig.4 Astronomical time scale for Cretaceous strata, ICDP boreholes SK-1, SK-2, SK-3 in the Songliao Basin

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松辽盆地白垩纪综合年代地层格架

Integrated chronostratigraphic framework for Cretaceous strata in the Songliao Basin

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