鄂尔多斯盆地早侏罗世富县期沉积演化: 大洋缺氧事件前后陆地气候变化的响应<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2022.04.056

古地理学报 ›› 2022, Vol. 24 ›› Issue (4): 697-712. doi: 10.7605/gdlxb.2022.04.056

• 岩相古地理学及沉积学 • 上一篇下一篇

鄂尔多斯盆地早侏罗世富县期沉积演化: 大洋缺氧事件前后陆地气候变化的响应^*

李昌昊^1,2, 葛禹^1,2, 金鑫^1,2, 时志强^1,2

1 成都理工大学沉积地质研究院,四川成都 610059;
2 成都理工大学油气藏地质及开发工程国家重点实验室,四川成都 610059

收稿日期:2021-12-22 修回日期:2022-03-03 出版日期:2022-08-01 发布日期:2022-08-09
通讯作者: 时志强,男,1972年生,成都理工大学沉积地质研究院教授。E-mail: szqcdut@163.com。
作者简介:李昌昊,男,1994年生,成都理工大学沉积地质研究院在读硕士研究生。E-mail: 634891625@qq.com。
基金资助:
*国家自然科学基金项目(编号: 41902106,41572085)资助

Sedimentological evolution during the Early Jurassic Fuxian period in Ordos Basin: palaeoclimatic response to Toarcian Oceanic Anoxic Event

LI Changhao^1,2, GE Yu^1,2, JIN Xin^1,2, SHI Zhiqiang^1,2

1 Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu 610059,China;
2 State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,China

Received:2021-12-22 Revised:2022-03-03 Online:2022-08-01 Published:2022-08-09
Contact: SHI Zhiqiang,born in 1972,is a professor of Institute of Sedimentary Geology,Chengdu University of Technology.E-mail: szqcdut@163.com.
About author:LI Changhao,born in 1994,is a master degree student in Institute of Sedimentary Geology,Chengdu University of Technology. E-mail: 634891625@qq.com.
Supported by:
National Natural Science Foundation of China(Nos. 41902106,41572085)

摘要/Abstract

摘要： 托阿尔期早期早侏罗世大洋缺氧事件(T-OAE,~183.8 Ma)是一次全球性的地质事件,鄂尔多斯盆地下侏罗统富县组记录了此次地质事件的陆地响应过程。主要基于盆地东缘野外地质调查、扫描电镜及薄片分析,本次研究描述了盆地东北部富县组岩性、颜色和沉积序列,利用前人研究成果总结了富县期岩相古地理变化规律及沉积模式,认为富县期经历了由干旱到湿润的古气候变化: 富县组下部含植物化石较为丰富的白色砂砾岩及黑色、灰色泥页岩沉积于湿润气候时期,对应着盆地下切河谷发育期和填平补齐期; 而上覆的罕见植物化石的杂色、红色泥页岩为(富县期晚期)相对平坦地形条件下的沉积,对应着早、中侏罗世湿润气候背景下的一次干旱气候脉动,为托阿尔期大洋缺氧事件在陆相环境的气候响应,可由此进行富县组区域等时性对比。研究认为“粗富县”为下切谷内河流充填沉积, “细富县”形成于湖泊环境或河漫环境, “黑富县”和“白富县”是湿润气候条件下沉积产物,而“红富县”和“杂富县”为T-OAE期后干旱条件下形成。

关键词: 侏罗纪古气候, 富县组, 托阿尔期海洋缺氧事件, 岩相古地理, 鄂尔多斯盆地

Abstract: As a global geological event,the early Toarcian(Early Jurassic)Oceanic Anoxic Event(T-OAE)(~183.8 Ma)affected both the marine and terrestrial environments. The response of this event had been recorded in the Lower Jurassic Fuxian Formation in the Ordos Basin. Based on the field geological survey,scanning electron microscopy and thin section analysis,we studied the lithology,color changes and sedimentary sequence of the Fuxian Formation in the northeastern Order Basin. Together with the previous research results of literature,we revealed the lithofacies palaeogeography and sedimentary model of the Fuxian period. Our results show that the Ordos Basin had experienced the palaeoclimatic change from wet to drought during the Fuxian period. The white glutenite and black or gray mudstone/shale containing abundant plant fossils deposited in the humid conditions,which corresponds to the filling stage of valleys in the basin. After filling up,the variegated and red mudstone/shale containing few plant fossils deposited in the flat topographical condition during the late Fuxian period,corresponding to an arid climate pulse under the overall humid climate in the Early and Middle Jurassic periods. The changes of rock color and climate are interpreted as the continental response of the T-OAE,which can be used for the isochronous correlation of the Fuxian Formation. We interpret the “coarse Fuxian”was fluvial deposits filling the incised valleys,the “fine Fuxian”deposited in lake or flood plain environments,the “black Fuxian”and “white Fuxian”were sedimentary products of humid climate,while “variegated Fuxian”and “red Fuxian”deposited under drought climate condition after the T-OAE.

Key words: Jurassic palaeoclimate, Fuxian Formation, Toarcian Oceanic Anoxic Event(T-OAE), lithofacies palaeogeography, Ordos Basin

中图分类号:

P588.2
P532

李昌昊, 葛禹, 金鑫, 时志强. 鄂尔多斯盆地早侏罗世富县期沉积演化: 大洋缺氧事件前后陆地气候变化的响应^*[J]. 古地理学报, 2022, 24(4): 697-712.

LI Changhao, GE Yu, JIN Xin, SHI Zhiqiang. Sedimentological evolution during the Early Jurassic Fuxian period in Ordos Basin: palaeoclimatic response to Toarcian Oceanic Anoxic Event[J]. JOPC, 2022, 24(4): 697-712.

http://www.gdlxb.cn/CN/Y2022/V24/I4/697

参考文献

[1] 卜广平,陈朝兵,成健,柴慧强,李海菲,唐栋梁. 2019. 胡尖山地区前侏罗纪古地貌及成藏条件分析. 断块油气田, 26(1): 1-6.
[Bu G P,Chen C B,Cheng J,Chai H Q,Li H F,Tang D L.2019. Pre-Jurassic paleogeomorphology and formation conditions of reservoirs in Hujianshan area. Fault-Block Oil & Gas Field, 26(1): 1-6]
[2] 陈洪德,赵俊兴,付锁堂,倪新锋. 2007. 鄂尔多斯盆地中南部早中侏罗世沉积层序充填动力学作用过程. 天然气工业, 27(5): 21-25,147-148.
[Chen H D,Zhao J X,Fu S T,Ni X F.2007. Sedimentary sequence filling dynamic process of early-middle Jurassic in south-central Ordos Basin. Natural Gas Industry, 27(5): 21-25,147-148]
[3] 陈兰,伊海生,夏敏全,邹艳荣. 2007. 藏北双湖地区早Toarcian期大洋缺氧事件: 沉积学、古生物学及地球化学特征. 生态学杂志, 26(11): 1793-1797.
[Chen L,Yi H S,Xia M Q,Zhou Y R.2007. Early Toarcian oceanic anoxic event in the Shuanghu area,northern Tibet: sedimentology,palaeobiology and geochemistry. Chinese Journal of Ecology, 26(11): 1793-1797]
[4] 陈庸勋,戴东林,杨昌贵. 1981. 岩相古地理研究方法: 以鄂尔多斯盆地为例. 北京: 地质出版社.
[Chen Y X,Dai D L,Yang C G.1981. The Research Method of Lithofacies Paleogeography: Takes Ordos Basin As an Example.Beijing: Geology Publishing House]
[5] 戴福贵,刘宝睿,杨克绳. 2008. 华北盆地地震剖面地质解释及其构造演化. 中国地质, 35(5): 820-840.
[Dai F G,Liu B R,Yang K S.2008. Geological interpretation of seismic sections and tectonci evolution of the North China Basin. Geology in China, 35(5): 820-840]
[6] 邓胜徽. 2007. 中生代主要植物化石的古气候指示意义. 古地理学报,9(6): 559-574.
[Deng S H.2007. Palaeoclimatic implications of main fossil plants of the Mesozoic. Journal of Palaeogeography(Chinese Edition),9(6): 559-574]
[7] 邓胜徽,卢远征,樊茹,方林浩,李鑫,刘璐. 2012. 早侏罗世Toarcian期大洋缺氧事件及其在陆地生态系统中的响应. 地球科学,37(S2): 23-38.
[Deng S H,Lu Y Z,Fan R,Fang L H,Li X,Liu L.2012. Toarcian(Early Jurassic)Oceanic anoxic event and the response in terrstirial ecosystem. Earth Science,37(S2): 23-38]
[8] 邓胜徽,商平,卢远征,赵怡,李鑫,樊茹,董淑欣. 2015. 内蒙古锡林浩特盆地早侏罗世晚期植物群: 兼论中国早侏罗世晚期气候. 古地理学报, 17(5): 617-634.
[Deng S H,Shang P,Lu Y Z,Zhao Y,Li X,Fan R,Dong S X.2015. A late Early Jurassic flora from Xilinhot Basin of Inner Monogolia,with discussions on coeval climate in China. Journal of Palaeogeography(Chinese Edition), 17(5): 617-634]
[9] 冯宝华. 1988. 彬县延长群古风化壳、富县组“花斑泥岩”和华池等地富县组粘土岩的特征及相变关系. 煤田地质与勘探,(3): 12-14.
[Feng B H.1988. Characteristice and phase change relationship of paleoweathering crust of Yanchang Group in Binxian,“Porphyry mudstone”of Fuxian Formation and claystone of Fuxian Formation in Huachi and other places. Coal Geology & Exploration,(3): 12-14]
[10] 冯云鹤. 2014. 鄂尔多斯盆地(内蒙古部分)富县组的发现及其意义. 地层学杂志, 38(4): 449-453.
[Feng Y H.2014. The discovery of the Fuxian Formation in the Ordos Basin(Inner Mongolia Part)and its implications. Journal of Stratigraphy, 38(4): 449-453]
[11] 冯增昭,鲍志东,康祺发,张永生,谭健,李振亚,庞福民,赵学仁. 1999. 鄂尔多斯早古生代古构造. 古地理学报, 1(2): 84-91.
[Feng Z Z,Bao Z D,Kang Q F,Zhang Y S,Tan J,Li Z Y,Pang F M,Zhao X R.1999. Early Paleozoic paleostructure in Ordos Basin. Journal of Palaeogeography(Chinese Edition), 1(2): 84-91]
[12] 葛道凯,杨起,付泽明,李祯,李宝芳. 1989. 陕北榆林富县组中的遗迹化石及其环境意义. 煤田地质与勘探,(6): 1-3,77.
[Ge D K,Yang Q,Fu Z M,Li Z,Li B F.1989. The trace fossil and depositional environment of Fuxian Formation,Yulin Country,Northern Shaanxi Province. Coal Geology & Exploration,(6): 1-3,77.]
[13] 葛道凯,杨起,付泽明,李祯. 1991. 陕西榆林侏罗纪煤系基底古侵蚀面的地貌特征及其对富县组沉积作用的控制. 沉积学报, 9(3): 65-73.
[Ge D K,Yang Q,Fu Z M,Li Z.1991. The palaeomorphologic features of the basement of the Jurassic coal measures and its control on the sedimentation of Fuxian Formation in Yulin,Shaanxi. Acta Sedimentologica Sinica, 9(3): 65-73]
[14] 高选政. 1996. 鄂尔多斯盆地早侏罗世岩相古地理. 煤田地质与勘探, 24(3): 1-5.
[Gao X Z.1996. Lithofacies paleogeography of early Jurassic in Ordos Basin. Coal Geology & Exploration, 24(3): 1-5]
[15] 郭正权,张立荣,楚美娟,黄锦绣. 2008. 鄂尔多斯盆地南部前侏罗纪古地貌对延安组下部油藏的控制作用. 古地理学报, 10(1): 63-71.
[Guo Z Q,Zhang L R,Chu M J,Huang J X.2008. Pre-Jurassic palaeogeomorphic control on the hydrocarbon accumulaton in the Lower Yan'an Formation in southern Ordos Basin. Journal of Palaeogeography(Chinese Edition), 10(1): 63-71]
[16] 何善斌,马世东,刘小宁. 2008. 鄂尔多斯南部侏罗系中下统沉积特征及演化规律. 石油天然气学报, 30(3): 170-171,449.
[He S B,Ma S D,Liu X N.2008. The depositional characteristics and evolution rules of the Middle and Lower Jurassic in the South of Ordos Basin. Journal of Oil and Gas Technology, 30(3): 170-171,449]
[17] 胡广,曹剑,胡文瑄,姚素平,刘文汇. 2014. 大洋缺氧事件及其等时陆相沉积与烃源岩发育. 西南石油大学学报(自然科学版), 36(5): 1-15.
[Hu G,Cao J,Hu W X,Yao S P,Liu W H.2014. Forntiers of the Oceanic Anoxic Event(OAEs),terrsetrial deposits and development of source rocks. Joural of Southwest Petroleum University(Science and Technology Edition), 36(5): 1-15]
[18] 胡修棉. 2015. 东特提斯洋晚中生代—古近纪重大事件研究进展. 自然杂志, 37(2): 93-102.
[Hu X M.2015. Overview of the Late Mesozoic Paleogene major paleoceanographic and geological event in Eastern Tethyan Ocean. Chinese Journal of Nature, 37(2): 93-102]
[19] 胡修棉,李娟,韩中,李永祥. 2020. 中新生代两类极热事件的环境变化、生态效应与驱动机制. 中国科学: 地球科学, 50(8): 1023-1043.
[Hu X M,Li J,Han Z,Li Y X.2020. Two types of hyperthermal events in the Mesozoic-Cenozoic: environmental impacts,biotic effects,and driving mechanisms. Science China Earth Sciences, 50(8): 1023-1043]
[20] 黄迪颖. 2019. 中国侏罗纪综合地层和时间框架. 中国科学: 地球科学, 49(1): 227-256.
[Huang D Y.2019. Jurassic integrative stratigraphy and timescale of China. Science China Earth Sciences, 49(1): 227-256]
[21] 黄克难,詹家祯,邹义声,王智,周春梅,肖继南. 2003. 新疆库车河地区三叠系和侏罗系沉积环境及古气候. 古地理学报, 5(2): 197-208.
[Huang K N,Zhan J Z,Zou Y S,Wang Z,Zhou C M,Xiao J N.2003. Sedimentary environments and Palaeoclimate of the Triassic and Jurassic in Kuqa River area,Xinjiang. Journal of Palaeogeography(Chinese Edition), 5(2): 197-208]
[22] 黄枝高,周惠琴. 1980. 古植物. 见: 中国地质科学院地质研究所. 陕甘宁盆地中生代地层古生物(1). 北京: 地质出版社,43-114.
[Huang Z G,Zhou H Q.1980. Palaeobotany. In: Institute of Geology,Chinese Academy of Geological Sciences.Mesozoic Stratigraphic paleontology in Shaanxi-Gansu-Ningxia Basin(1). Beijing: Geology Publishing House,43-114]
[23] 贾建称,贾茜,张妙逢,吴艳,陈晨. 2015. 鄂尔多斯盆地西南缘侏罗系鄂尔多斯盆地西南缘侏罗系—下白垩统划分对比与煤炭开发区划研究. 中国煤炭地质, 27(7): 29-36.
[Jia J C,Jia Q,Zhang M F,Wu Yan,Chen C.2015. A study on Jurassic to Lower Cretaceous stratigraphic division,correlation and coal exploitation regionalization in southwestern margin of Ordos Basin. Coal Geology of China, 27(7): 29-36]
[24] 蒋代琴,文志刚,汤仁文,贺彤彤. 2018. 鄂尔多斯盆地吴起地区古地貌对侏罗系下部油藏形成和富集控制机制分析. 地质力学学报, 24(5): 627-634.
[Jiang D Q,Wen Z G,Tang R W,He T T.2018. Analysis on the formation and enrichment control mechanism of the Lower Jurassic reservoirs by paleo-geomorphology of Wuqi area in the Ordos Basin. Journal of Geomechanics, 24(5): 627-634]
[25] 旷理雄,梁力文,敬小军,史德锋,黄文俊. 2012. 从前侏罗纪古地貌的角度论鄂尔多斯盆地靖边—鄂托克前旗地区油气成藏模式. 中国有色金属学报, 22(3): 837-843.
[Kuang L X,Liang L W,Jing X J,Shi D F,Huang W J.2012. Accumulation model of Jingbian-Etuokeqianqi area in Ordos Basin from angle of pre-Jurassic palaeogeomorphology. The Chinese Journal of Nonferrous Metal, 22(3): 837-843]
[26] 李宝芳,李祯,林畅松,温显端,付泽明,周慧堂. 1995. 鄂尔多斯盆地中部下侏罗统沉积体系和层序地层. 北京: 地质出版社, 27-87.
[Li B F,Li Z,Lin C S,Wen X D,Fu Z M,Zhou H T.1995. Sedimentary System and Sequence Stragraphy of Lower Jurassic in Central Ordos Basin. Beijing: Geology Publishing House,27-87]
[27] 李旦,葛芷渊,程小兵. 2006. 志丹油田侏罗纪沉积前古地貌特征与延10油藏分布. 西北地质, 39(3): 55-58.
[Li D,Ge Z Y,Cheng X B.2006. Controls of palaeogeomorphy on Yan'an Formation reservior before Jurassic deposition and reservoir characteristice in Zhidan Oil Field. Northwestern Geology, 39(3): 55-58]
[28] 李钝,王万佑. 1987. 彬县矿区富县组“花斑泥岩”成因分析. 煤田地质与勘探,(1): 10-12.
[Li D,Wang W Y.1987. Genetic analysis of “Mosaic mudstone”of Fuxian Formation in Binxian Mining area. Coal Geology & Exploration,(1): 10-12]
[29] 李凤杰,李磊,林洪,杨豫川,方朝刚,孟立娜. 2013. 鄂尔多斯盆地吴起地区侏罗系侵蚀古河油藏分布特征及控制因素. 天然气地球科学, 24(6): 1109-1117.
[Li F J,Li L,Lin H,Yang Y C,Fang C G,Meng L N.2013. Distribution characteristice and controling factors analyses on incised paleochannel reservior of valley filling in Jurassic of Wuqi area, Ordos Basin. Natural Gas Geoscience, 24(6): 1109-1117]
[30] 李元昊,杨桂茹,彭建,郑亚军,王茜,何拓平. 2020. 鄂尔多斯盆地前侏罗纪古地貌形成演化及沉积充填特征. 世界地质, 39(1): 56-71.
[Li Y H,Yang G R,Peng J,Zheng Y J,Wang Q,He T P.2020. Formation and evolution of pre-Jurassic palaeogeomorphology and characteristice of sedimentary filling in Ordos Basin. Global Geology, 39(1): 56-71]
[31] 李智民,陈磊,温道明. 1985. 陕北侏罗纪煤田榆横地区延安组沉积环境分析和聚煤特征. 陕西地质, 3(2): 15-30.
[Li Z M,Chen L,Wen D M.1985. Sedimentary environment analysis and coal accumulation characteristic of Yan'an Formation in Yuheng area during Jurassic in northern Shaanxi. Geology of Shaanxi, 3(2): 15-30]
[32] 刘池洋,赵红格,桂小军,岳乐平,赵俊峰,王建强. 2006. 鄂尔多斯盆地演化—改造的时空坐标及其成藏(矿)响应. 地质学报,80(5): 617-638.
[Liu C Y,Zhao H G,Gui X J,Yue L P,Zhao J F,Wang J Q.2006. Space-time coordinate of the evolution and reformation and mineralization response in Ordos Basin. Acta Geologica Sinica,80(5): 617-638]
[33] 刘嘉. 2014. 靖边南部前侏罗纪古地貌特征及其控制作用. 辽宁化工, 43(12): 1530-1533.
[Liu J.2014. Pre-Jurassic paleogeomophology characteristics and control function in the South of Jingbian. Liaoning Chemical Industry, 43(12): 1530-1533]
[34] 刘犟,李凤杰,侯景涛,方朝刚,孟立娜. 2012. 鄂尔多斯盆地吴起地区下侏罗统富县组沉积相特征. 岩性油气藏, 24(3): 74-78.
[Liu J,Li F J,Hou J T,Fang C G,Meng L N.2012. Sedimentary facies of the Lower Jurasic Formation in Wuqi area,Ordos Basin. Lithologic Reservoirs, 24(3): 74-78]
[35] 刘魁梧. 1991. 古气候的影响因素及恢复标志. 国外地质(北京),(1): 5-10.
[Liu K W.1991. Influencing factors and signs of restoration about palaeoclimate. Foreign Geoexploration Technology(Beijing),(1): 5-10]
[36] 刘瑞东,王宝清,王博,狄翔,郭斌,刘伟. 2014. 鄂尔多斯盆地环江地区前侏罗纪古地貌恢复研究. 石油地质与工程, 28(5): 9-11,15,153.
[Liu R D,Wang B Q,Wang B,Di X,Guo B,Liu W.2014. Study on pre-Jurassic palaeogeomorphology reconstruction of Huanjiang region,Ordos Basin. Petroleum Geology and Engineering, 28(5): 9-11,15,153.]
[37] 刘若,吴一民. 1985. 焦坪矿区富县组“花斑泥岩”沉积环境初探. 煤田地质与勘探,(2): 3-8,73.
[Liu R,Wu Y M.1985. Preliminary study on the sedimentary environment of “Mosaic mudstone”of Fuxian Formation in Jiaoping mining area. Coal Geology & Exploration,(2): 3-8,73.]
[38] 刘秀铭,吕镔,毛学刚,温昌辉,俞鸣同,郭雪莲,陈家胜,王涛. 2014. 风积地层中铁矿物随环境变化及其启示. 第四纪研究, 34(3): 443-457.
[Liu X M,Lü B,Mao X G,Wen C H,Yu M T,Guo X L,Chen J S,Wang T.2014. Iron minerals of aeolian deposits vary with environment and its significances. Quaternary Sciences, 34(3): 443-457]
[39] 刘玄春. 2018. 鄂尔多斯盆地环县地区侏罗系富县组—延10油层组古地貌分析及沉积相特征研究. 成都理工大学硕士学位论文: 1-73.
[Liu X C.2018. Palaeogeomorphology analysis and Sedimentary facies characteristics of Jurassic Fuxian Formaion and Yan'an Oil Formaion in Huanxian area,Ordos Basin. Masteral dissertation of Chengdu University of Technology: 1-73]
[40] 毛学刚,刘秀铭. 2016. 浅析中元古界和白垩系红层中泥裂的特征和古环境意义. 亚热带资源与环境学报, 11(3): 20-28.
[Mao X G,Liu X M.2016. Preliminary analysis on characterization of mud-cracks in Meso-proterozoic red beds and Cretaceous Danxia red beds and their palo-enviromental implications. Journal of Subtropical Resources and Environment, 11(3): 20-28]
[41] 孟繁松. 2010. 中国南方海、陆相侏罗系的划分与对比. 华南地质与矿产,(4): 55-65.
[Meng F S.2010. Stratigraphic division and correlation of the marine and continental Jurassic System in south China. Geology and Mineral Resources of South China,(4): 55-65]
[42] 孟立娜,李凤杰,方朝刚,李磊,林洪. 2012. 鄂尔多斯盆地吴起地区侏罗纪早中期河流沉积及油气分布. 西安石油大学学报(自然科学版), 27(6): 1-8.
[Meng L N,Li F J,Fang C G,Li L,Lin H.2012. Study on fluvial deposits and oil and gas distribution of early and middle Jurassic in Wuqi area,Ordos Basin. Journal of Xi'an Shiyou University(Natural Science Edition), 27(6): 1-8]
[43] 邱若原,方琳浩,卢远征,邓胜徽,张新智,吕沛宗,任嘉豪,黄汝婷,房亚男,张小宇,李宏佳,鲜本忠,师生宝. 2021. 早侏罗世缺氧事件在塔里木盆地的响应. 沉积学报. https: //doi. 10.14027/j.issn.1000-0550.2021.095.
[Qiu R Y,Fang L H,Lu Y Z,Deng S H,Zhang X Z,Lü P Z,Ren J H,Huang R T,Fang Y N,Zhang X Y,Li H J,Xian B Z,Shi S B.2021. Response to the Early Jurassic oceanic anoxic events in the Tarim Basin. Acta Sedimentologica Sinica. https: //doi. 10.14027/j.issn.1000-0550.2021.095]
[44] 时志强,韩永林,张锦泉. 2001. 鄂尔多斯盆地早侏罗世富县期岩相古地理特征. 矿物岩石, 21(3): 124-127.
[Shi Z Q,Han Y L,Zhang J Q.2001. Lithofacies paleogeography of Fuxian stage in Early Jurassic in Ordos Basin.Mineralogy Petrology, 21(3): 124-127]
[45] 时志强,韩永林,赵俊兴. 2002. 鄂尔多斯盆地早侏罗世富县期冲积扇沉积. 成都理工学院学报, 29(4): 390-393.
[Shi Z Q,Han Y L,Zhao J X.2002. Fans at the Early Jurassic Fuxian stage in Ordos Basin. Journal of Chengdu University of Technology, 29(4): 390-393]
[46] 阎存凤. 1992陕西榆林—横山地区富县组孢粉组合. 植物学报,(8): 634-640,653-654.
[Yan C F.1992. The sporo-pollen assemblage from Fuxian Formation in Yulin-Hengshan region,Shaanxi Province. Journal of Integrative Plant Biology,(8): 634-640,653-654]
[47] 袁伟,周晓星,武富礼,赵思远. 2014. 鄂尔多斯盆地白河区早中侏罗世沉积相及其与油气运聚的关系. 石油地质与工程, 28(2): 1-4,145.
[Yuan W,Zhou X X,Wu F L,Zhao S Y.2014. Early-middle Jurassic sedimentary facies and its relationship with the hydrocarbon migration and accumulation in Baihe area of Ordos Basin. Petroleum Geology and Engineering, 28(2): 1-4,145]
[48] 袁效奇,傅智雁,王喜富. 2003. 中国北方侏罗系(V)鄂尔多斯地层区. 北京: 石油工业出版社,54-94.
[Yuan X Q,Fu Z Y,Wang X F.2003. Jurassic system in northern China(V)Ordos stratigraphic region. Beijing: Petroleum Industry Press,54-94]
[49] 曾传富,田景春,张涛,刘哲,王峰. 2015. 镇北地区前侏罗纪古地貌特征与油气富集规律研究. 断块油气田, 22(3): 273-277.
[Zeng C F,Tian J C,Zhang T,Liu Z,Wang F.2015. Characteristics of pre-Jurassic palaeogeomorphology and hydrocarbon accumulation regularity in Northern Zhenyuan area. Fault-Block Oil & Gas Field, 22(3): 273-277]
[50] 张泓,李恒堂,熊存卫. 1998. 中国西北侏罗纪含煤地层聚煤规律. 北京: 地质出版社,1-317.
[Zhang H,Li H T,Xiong C W.1998. Coal Accumulation Regularity of Jurassic Coal-bearing Strata in Northwest China. Beijing: Geology Publishing House, 1-317]
[51] 张泓,晋香兰,李贵红,杨志远,张慧,贾建称. 2008. 鄂尔多斯盆地侏罗纪—白垩纪原始面貌与古地理演化. 古地理学报, 10(1): 1-11.
[Zhang H,Jin X L,Li G H,Yang Z Y,Zhang H,Jia J C.2008. Original features and palaeogeographic evolution during the Jurassic-Cretaceous in Ordos Basin. Journal of Palaeogeography(Chinese Edition), 10(1): 1-11]
[52] 张雪映,剡鹏兵,王贵. 2021. 鄂尔多斯盆地北部延安组沉积学特征与成矿潜力分析. 铀矿地质, 37(2): 171-181.
[Zhang X Y,Yan P B,Wang G.2021. Sedimentary characteristics and metallogenic potential of Yan'an Formation in the north of Ordos Basin. Uranium Geology, 37(2): 171-181]
[53] 赵虹,党犇,党永潮,王小军,吴娜,杨骁,王宇. 2020. 鄂尔多斯盆地安塞志丹地区侏罗系延安组下部组合沉积演化及其对油气的控制. 西北大学学报(自然科学版), 50(3): 490-500.
[Zhao H,Dang B,Dang Y C,Wang X J,Wu N,Yang X,Wang Y.2020. Depositional system and its evolution of the Lower Yan'an Formation Jurassic in Ansai district,Ordos Basin. Journal of Northwest University(Natural Science Edition), 50(3): 490-500]
[54] 赵俊兴,陈洪德. 2006. 鄂尔多斯盆地侏罗纪早中期甘陕古河的演化变迁. 石油与天然气地质. 27(2): 152-158.
[Zhao J X,Chen H D.2006. Evolution of Gan-Shaan paleochannel during Early and Middle Jurassic in Ordos Basin. Oil & Gas Geology, 27(2): 152-158]
[55] 赵俊兴,陈洪德,杨华,付锁堂,付金华,同晓荣. 2005. 鄂尔多斯中南部中下侏罗统储层成因类型与油气聚集关系. 成都理工大学学报(自然科学版), 32(3): 246-251.
[Zhao J X,Chen H D,Yang H,Fu S T,Fu J H,Tong X R.2005. Genetic types and their relationship with oil gas accumulation of the Lower and Middle Jurassic reservoirs in Ordos Basin,China. Journal of Chengdu University of Technology(Science & Technology Edition), 32(3): 246-251]
[56] 赵俊兴,陈洪德,张锦泉. 1999. 鄂尔多斯盆地下侏罗统富县组沉积体系及古地理. 岩相古地理, 19(5): 40-46.
[Zhao J X,Chen H D,Zhang J Q.1999. The depositiona systems and palaeogeography of the Lower Jurassic Fuxian Formaion in the Ordos Basin. Sedimentary Facies and Palaeogeography, 19(5): 40-46]
[57] 赵敏,王多云,刘军锋,孟祥宏,李树同,焦健. 2010. 沉积前古地貌对油藏成藏的有利条件分析: 以鄂尔多斯盆地子午岭地区下侏罗统为例. 天然气地球科学, 21(3): 476-481.
[Zhao M,Wang D Y,Liu J F,Meng X H,Li S T,Jiao J.2010. Favorable conditions for petroleum accumulation by paleogeomorphology before deposition: taking Lower Jurassic in Ziwuling Area,Ordos Basin as an example. Nature Gas Geoscience, 21(3): 476-481]
[58] 中国煤田地质总局. 1996. 鄂尔多斯盆地聚煤规律及煤炭资源评价. 北京: 煤炭工业出版社, 33-37,187.
[China National Administration of Coal Geology. 1996. Coal Accumulation Law and Coal Resource Evaluation in Ordos Basin. Beijing: Coal Industry Publishing House,33-37,187]
[59] Baker S J,Hesselbo S P,Lenton T M,Duarte L V,Belcher C M.2017. Charcoal evidence that rising atmospheric oxygen terminated Early Jurassic ocean anoxia. Nature Communications, 8(1): 1-7.
[60] Boulila S,Galbrun B,Huret E,Hinnov L A,Rouget I,Gardin S,Bartolini A.2014. Astronomical calibration of the Toarcian Stage: implications for sequence stratigraphy and duration of the early Toarcian OAE. Earth and Planetary Science Letters, 386: 98-111.
[61] Caruthers A H,Smith P L,Gröcke D R.2014. The Pliensbachian-Toarcian(Early Jurassic)extinction: a north American perspective. Geological Society of America Special Papers, 505: 225-243.
[62] Caswell B A,Coe A L,Cohen A S.2009. New range data for marine invertebrate species across the early Toarcian(Early Jurassic)mass extinction. Journal of the Geological Society, 166: 859-872.
[63] Chen L,Yi H S,Zhong H,Hu R Z,Yin J R,Yang J K.2006. The calcareous nannofossil record and its geological significance in the Jurassic black shales from the Qiangtang Basin,northern Tibetan Plateau. Progress in Natural Science, 16(Special Issue): 264-273.
[64] Danise S,Twitchett R J,Little C T.2015. Environmental controls on Jurassic marine ecosystems during global warming. Geology, 43: 263-266.
[65] Dera G,Pellenard P,Neige P,Deconinck J F,Pucéat E,Dommergues J L.2009. Distribution of clay minerals in Early Jurassic Peritethyan seas: palaeoclimatic significance inferred from multiproxy comparisons. Palaeogeography, Palaeoclimatology, Palaeoecology, 271: 39-51.
[66] Gröcke D R,Hori R S,Trabucho-Alexandre J,Kemp D B,Schwark L.2011. Anopen ocean record of the Toarcian oceanic anoxic event. Solid Earth, 2: 245-257.
[67] Han Z,Hu X M,Kemp D B,Li J.2018. Carbonate-platform response to the Toarcian Oceanic Anoxic Event in the southern hemisphere: implications for climatic change and biotic platform demise. Earth and Planetary Science Letters, 489: 59-71.
[68] Haq B U.2018. Jurassic sea-level variations: a reappraisal. GSA Today, 28: 4-10.
[69] Hesselbo S P,Pienkowski G.2011. Stepwise atmospheric carbon-isotope excursion during the Toarcian Oceanic Anoxic Event(Early Jurassic,Polish Basin).Earth and Panetary Science Lettsers, 301(1): 365-372.
[70] Hesselbo S P,Jenkyns H C,Duarte L V,Duarte L V.2007. Carbon-isotope record of the Early Jurassic(Toarcian)Oceanic Anoxic Event from fossil wood and marine carbonate(Lusitanian Basin,Portugal).Earth and Planetary Science Letters, 253: 455-470.
[71] Hesselbo S P,Grocke D R,Jenkyns H C,Bjerrum C J,Farrimond P,Morgans B H S,Green.2000. Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event. Nature, 406: 392-395.
[72] Huang C J,Hesselbo S P.2014. Pacing of the Toarcian Oceanic Anoxic Event(Early Jurassic)from tronomical correlation of Marine sections. Gondwana Research, 25: 1348-1356.
[73] Idoia R,Antonio B,Antonio G,Ana S,Maider A,José M L G.2018. Isotope records(C-O-Sr)of late Pliensbachian-early Toarcian environmental perturbations in the westernmost Tethys(Majorca Island,Spain). Palaeogeography,Palaeoclimatology, Palaeoecology, 497: 168-185.
[74] Izumi K A,Miyaji T B,Tanabe K A.2012. Early Toarcian(Early Jurassic)oceanic anoxic event recorded in the shelf deposits in the northwestern Panthalassa: evidence from the Nishinakayama Formation in the Toyora area,west Japan(Article). Palaeogeography,Palaeoclimatology,Palaeoecology, 315-316: 100-108.
[75] Jenkyns H C.1985. The early Toarcian and Cenomanian-Turonian anoxic events in Europe: comparisons and contrasts. Geologische Rundschau, 74(3): 505-518.
[76] Jenkyns H C.1988. The early Toarcian(Jurassic)anoxic event;stratigraphic,sedimentary and geochemical evidence. American Journal of Science, 288(2): 101-151.
[77] Jin X,Shi Z Q,Barany V,Kemp D B,Han Z,Luo G M,Hu J F,He F,Chen L,Preto N.2020. The Jenkyns Event(early Toarcian OAE)in the Ordos Basin,North China. Global & Planetary Change, 193: 103273.
[78] Kemp D B,Coe A L,Cohen A S,Schwark L.2005. Astronomical pacing of methane release in the Early Jurassic period. Nature, 437: 396-399.
[79] Kemp D B,Coe A L,Cohen A S,Weedon G P.2011. Astronomical forcing and chronology of the early Toarcian(Early Jurassic)oceanic anoxic event in Yorkshire,UK. Paleoceanography, 26(4): 4210-4226.
[80] Liu M,Sun P,Them II T R,Theodore R,Li Y F,Sun S L,Gao X Y,Huang X,Tang Y J.2020. Organic geochemistry of a lacustrine shale across the Toarcian Oceanic Anoxic Event(Early Jurassic)from NE China. Global and Planetary Change, 191: 103214.
[81] McArthur J M.2007. Comment on “Carbon-isotope record of the Early Jurassic(Toarcian)Oceanic Anoxic Event from fossil wood and marine carbonate(Lusitanian Basin,Portugal)” by Hesselbo S,Jenkyns H C,Duarte L V and Oliveira L C V. Earth and Planetary Science Letters, 259(3): 634-639.
[82] McElwain J C,Wade-Murphy J,Hesselbo S P.2005. Changes in carbon dioxide during an oceanic anoxic event linked to intrusion into Gondwana coals. Nature, 435(7041): 479-482.
[83] Suan G,Pittet B,Bour I,Mattioli E,Duarte L,Mailliot S.2008. Duration of the Early Toarcian carbon isotope excursion deducedfrom spectral analysis: consequence for its possible causes. Earth and Planetary Science Letters, 267: 666-679.
[84] Trecalli A,Spangenberg J,Adatte T,Follmi K B,Parente M.2012. Carbonate platform evidence of ocean acidification at the onset of the early Toarcian oceanic anoxic event. Earth and Planetary Science Letters, 357(1): 214-225.
[85] Walker T R.1967. Formation of red beds in modern and ancient deserts.Geological Society of America Bulletin,78(3): 353-368.
[86] Wang Y D,Mosbrugger V,Zhang H.2005. Early to Middle Jurassic vegetation and climatic events in the Qaidam Basin,northwest China.Palaeogeography,Palaeoclimatology,Palaeoecology, 224(1): 200-216.
[87] Xu W M,Ruhl M,Jenkyns H C,Hesselbo S P,Riding J B,Selby D,Naafs B D A,Weijers J W H,Pancost R D,Tegelaar E W,Idiz E F.2017. Carbon sequestration in an expanded lake system during the Toarcian oceanic anoxic event.Nature Geoscience, 10(2): 129-134.

选择文件类型/文献管理软件名称

选择包含的内容

鄂尔多斯盆地早侏罗世富县期沉积演化: 大洋缺氧事件前后陆地气候变化的响应^*

Sedimentological evolution during the Early Jurassic Fuxian period in Ordos Basin: palaeoclimatic response to Toarcian Oceanic Anoxic Event

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	张晓阳, 窦云飞, 孔维江, 李康, 吕大炜, 陈金凤, 贾海波, 沈晓丽. 鄂尔多斯盆地东缘临兴地区本溪组铝土岩系沉积发育地质过程及储集层物性特征^*[J]. 古地理学报, 2025, 27(2): 286-306.
[2]	李阳. 鄂尔多斯盆地南缘旬探1井奥陶系天文旋回信号提取及三级层序的判识^*[J]. 古地理学报, 2025, 27(1): 209-224.
[3]	刘恒宇, 刘明洁, 郝志磊, 任茵, 吴恩郁, 许晗, 钟寿康, 谭秀成, 曾伟, 连承波, 戴鸿鸣. 古老深层致密砂岩储集层孔隙形成与保存机制:以鄂尔多斯盆地长城系为例^*[J]. 古地理学报, 2024, 26(6): 1435-1451.
[4]	刘明成, 吴胜和, 万晓龙, 李桢, 樊建民, 陈朝晖, 王梓沣, 刘海旭. 鄂尔多斯盆地庆城油田延长组页岩层系层序地层与沉积相特征^*[J]. 古地理学报, 2024, 26(4): 779-795.
[5]	魏柳斌, 王宗延, 李漪, 庞志超, 王前平, 包洪平, 杨琦琦, 王振, 苏中堂, 张立军. 豹皮(斑)状碳酸盐岩分类与成因初探: 以鄂尔多斯盆地马家沟组四段为例^*[J]. 古地理学报, 2024, 26(4): 880-894.
[6]	吴宇婷, 甯濛, 夏攀, 乔占峰, 于洲, 文华国. 白云岩-蒸发岩共生体系白云石化过程研究:以鄂尔多斯盆地马家沟组为例^*[J]. 古地理学报, 2024, 26(4): 895-910.
[7]	黄有根, 许杰, 郑小鹏, 刘燕, 钟寿康, 李琳, 张道锋, 谭秀成. 鄂尔多斯盆地中东部下二叠统太原组灰岩沉积特征与沉积模式^*[J]. 古地理学报, 2024, 26(4): 911-925.
[8]	李华, 何幼斌, 姚凤南, 何一鸣, 姜纯伟, 张显坤, 吴吉泽, 徐艳霞, 梁建设. 鄂尔多斯盆地西北缘奥陶系克里摩里组等深流沉积^*[J]. 古地理学报, 2024, 26(4): 962-971.
[9]	齐荣, 李国蓉, 张军涛, 王付斌, 李宇翔, 杨飞, 刘璐, 何赛, 田家奇, 李肖肖. 鄂尔多斯盆地富县地区马家沟组热液改造特征与研究意义^*[J]. 古地理学报, 2024, 26(3): 632-643.
[10]	丁晓琪, 田胤瑜, 雷涛, 张威, 李晓慧, 高景云. 吕梁古隆起对鄂尔多斯盆地马家沟组沉积的控制作用: 基于陕西府谷剖面^*[J]. 古地理学报, 2024, 26(3): 671-682.
[11]	李元昊, 史立川, 雷秀洁, 淡卫东. 鄂尔多斯盆地上三叠统延长组负载构造类型及特征^*[J]. 古地理学报, 2024, 26(2): 269-278.
[12]	刘国庆, 苏中堂, 郝志磊, 魏柳斌, 任军锋, 廖慧鸿, 吴浩文. 鄂尔多斯盆地马家沟组碳酸盐岩-膏盐岩共生体系沉积微相与沉积模式^*[J]. 古地理学报, 2024, 26(2): 279-295.
[13]	张忠民, 李依霖, 郑乃熙, 曹喆, 吕雪雁, 李宗峰, 孙润明, 夏昌盛, 李磊, 牛博, 宿宇驰, 张浩飞, 冯志强, 季汉成, 鲍志东. 北非地区Ghadames盆地早古生代岩相古地理演化特征^*[J]. 古地理学报, 2024, 26(1): 45-57.
[14]	熊加贝, 何登发, 成祥, 罗瑀峰. 鄂尔多斯盆地南缘奥陶系顶部碳酸盐岩风化壳特征及其成因机制^*[J]. 古地理学报, 2024, 26(1): 100-118.
[15]	毛丹凤, 何登发, 包洪平, 魏柳斌, 成祥, 苟钧壹, 石婧, 许艳华. 鄂尔多斯盆地怀远运动期不整合类型及其分布特征^*[J]. 古地理学报, 2024, 26(1): 119-131.

模态框（Modal）标题

选择文件类型/文献管理软件名称

选择包含的内容

鄂尔多斯盆地早侏罗世富县期沉积演化: 大洋缺氧事件前后陆地气候变化的响应*

Sedimentological evolution during the Early Jurassic Fuxian period in Ordos Basin: palaeoclimatic response to Toarcian Oceanic Anoxic Event

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

鄂尔多斯盆地早侏罗世富县期沉积演化: 大洋缺氧事件前后陆地气候变化的响应^*