早始新世温室气候与海侵作用对库车坳陷库姆格列木群含盐层系沉积的协同控制作用<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2024.03.052

古地理学报 ›› 2024, Vol. 26 ›› Issue (4): 926-940. doi: 10.7605/gdlxb.2024.03.052

• 岩相古地理学及沉积学 • 上一篇下一篇

早始新世温室气候与海侵作用对库车坳陷库姆格列木群含盐层系沉积的协同控制作用^*

张锡婷^1,2, 范坤宇³, 郭佩^1,2, 李鹏真³, 苗如霖^2,4, 邓宾^2,4

1 自然资源部深时地理环境重建与应用重点实验室,成都理工大学沉积地质研究院,四川成都 610059;
2 油气藏地质及开发工程国家重点实验室,成都理工大学,四川成都 610059;
3 中国石油塔里木油田公司勘探开发研究院,新疆库尔勒 652801;
4 成都理工大学能源学院,四川成都 610059

收稿日期:2023-05-04 修回日期:2023-10-25 出版日期:2024-08-01 发布日期:2024-07-29
通讯作者: 郭佩,女,1990年生,博士,副教授,主要从事咸化湖盆沉积与油气地质研究。E-mail: guopei18@cdut.edu.cn。
作者简介:张锡婷,女,1999年生,硕士研究生,地质学专业。E-mail: 1348167494@qq.com。
基金资助:
*国家自然科学基金项目(编号: 42272117,42002116)资助

Collaborative controls of the Early-Eocene greenhouse climates and transgression on deposition of salt-bearing sequence of Kumugeliemu Group in Kuqa Depression

ZHANG Xiting^1,2, FAN Kunyu³, GUO Pei^1,2, LI Pengzhen³, MIAO Rulin^2,4, DENG Bin^2,4

1 Key Laboratory of Deep-time Geography and Environment Reconstruction and Applications of Ministry of Natural Resources,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;
3 Research Institute of Exploration & Development PetroChina Tarim Oilfield Company,Xinjiang Korla 652801,China;
4 School of Energy,Chengdu University of Technology,Chengdu 610059,China

Received:2023-05-04 Revised:2023-10-25 Online:2024-08-01 Published:2024-07-29
Contact: GUO Pei,born in 1990,Ph.D.,is an associate professor. She is engaged in sedimentology and petroleum geology of saline lake basins. E-mail: guopei18@cdut.edu.cn.
About author:ZHANG Xiting, born in 1999, major in geology. E-mail: 1348167494@qq.com.
Supported by:
Financially supported by the National Natural Science Foundation of China(Nos. 42272117,42002116)

摘要/Abstract

摘要： 塔里木盆地北部库车坳陷库姆格列木群(54-46 Ma)厚层含盐层系为油气成藏的优质区域盖层,但该套含盐层系的原始时空展布、古地理环境和沉积控制因素尚不明确,给盐下油气藏钻井施工造成了较大困难。通过盆缘野外露头剖面实测与盆内录井元素分析相结合,开展盐湖中心与边缘沉积旋回对比研究,探讨库姆格列木群含盐层系发育的主控因素。库姆格列木群发育3个Ⅲ级旋回:第1个Ⅲ级旋回Ⅰ₁以盆缘砂砾岩—泥岩—石膏岩组合、湖盆中心泥岩—石膏岩—盐岩—碳酸盐岩组合为特征,指示陆内盆地向陆缘盆地的古地理环境转变。第2个Ⅲ级旋回Ⅰ₂以盆缘砂砾岩—泥岩—石膏岩组合、湖盆中心厚层盐岩加泥岩组合为特征,为陆缘盆地盐湖沉积模式。第3个Ⅲ级旋回Ⅰ₃盆缘—盆内沉积具有相似的膏质泥岩和泥岩组合特征,为陆内干盐湖沉积模式。结合早始新世全球气候和海平面升降变化历史,认为Ⅰ₁旋回(约54-51 Ma)由陆内向陆缘环境的转变及厚层石膏岩的沉积受早始新世气候适宜期(53-51 Ma)和全球海平面升高的影响,Ⅰ₂旋回(约51-48 Ma)厚层盐岩的沉积受全球持续干旱气候和海平面再次升高的影响,而Ⅰ₃旋回(约48-46 Ma)厚层含盐层系沉积的缺失与全球气候持续干旱和海平面下降有关。

关键词: 含盐层系, 物质来源, 陆缘盆地, 沉积旋回, 库姆格列木群, 库车坳陷, 塔里木盆地

Abstract: The thick salt-bearing sequence in Paleogene Kumugeliemu Group(54-46 Ma)of the Kuqa Depression acts as the high-quality regional caps for oil and gas accumulation. However,the original temporal-spatial distribution,palaeogeographic environment,and sedimentary controlling factors of the salt-bearing sequence remain unclear,which causes great difficulties for the drilling of the subsalt hydrocarbon reservoirs. Through the outcrop measurement at the basin margin and the logging element analysis within the basin,the correlation of sedimentary cycles between the lake-basin center and the margin was carried out to explore the main controlling factors of the salt-bearing sequence deposition of Kumugeliemu Group. The Kumugeliemu Group consists of three third-order cycles. The first third-order cycle Ⅰ₁ is characterized by the lithofacies assemblage of conglomerates,sandstones,mudstones and gypsums at basin margins,and of mudstones,gypsums,halites,carbonates at basin center,indicating an palaeogeographic-environment transformation from a terrigenous basin to a continental-margin basin. The second third-order cycle Ⅰ₂ is characterized by the lithofacies assemblage of conglomerates,sandstones,mudstones,and gypsums at basin margins and the assemblage of thick halites and minor mudstones at basin center,corresponding to a depositional model of a terrigenous epeiric basin. The third third-order cycle Ⅰ₃ has similar lithofacies assemblage at the lake-basin margin and center,characterized by thin layer gypseous mudstones and mudstones,typical depositional model of terrigenous playa lakes. Combined with the Early-Eocene global climates and sea-level changes,it is believed that the deposition of thick gypsum rocks of Ⅰ₁(ca. 54-51 Ma)were related to the Early Eocene Climatic Optimum(53-51 Ma)and global sea-level rise. The deposition of thick halite rocks in Ⅰ₂(ca. 51-48 Ma)was controlled by the global dry climate and sea-level rise. The absence of thick salt-bearing sequence deposits in Ⅰ₃(ca. 48-46 Ma)is related to the global dry climate and sea-level drops.

Key words: salt-bearing sequence, salt sources, epeiric basin, sedimentary cycle, Kumugeliemu Group, Kuqa Depression, Tarim basin

中图分类号:

P588.24+7

张锡婷, 范坤宇, 郭佩, 李鹏真, 苗如霖, 邓宾. 早始新世温室气候与海侵作用对库车坳陷库姆格列木群含盐层系沉积的协同控制作用^*[J]. 古地理学报, 2024, 26(4): 926-940.

ZHANG Xiting, FAN Kunyu, GUO Pei, LI Pengzhen, MIAO Rulin, DENG Bin. Collaborative controls of the Early-Eocene greenhouse climates and transgression on deposition of salt-bearing sequence of Kumugeliemu Group in Kuqa Depression[J]. JOPC, 2024, 26(4): 926-940.

http://www.gdlxb.cn/CN/Y2024/V26/I4/926

参考文献

[1] 曹养同,杨海军,刘成林,顾乔元,焦鹏程,卢玉红. 2010. 库车盆地古—新近纪蒸发岩沉积对喜马拉雅构造运动期次的响应. 沉积学报, 28(6): 1054-1065.
[Cao Y T,Yang H J,Liu C L,Gu Q Y,Jiao P C,Lu Y H.2010. Response on sediment of evaporate in Kuqa Basin from Paleogene to Neogene period and Himalayan tectonic phase. Acta Sedimentologica Sinica, 28(6): 1054-1065]
[2] 曹养同,刘成林,颜辉,焦鹏程,张华,吕凤琳,丁婷. 2016. 中—新生代塔里木与中亚盐湖链蒸发岩沉积及其控制因素初探. 矿床地质, 35(3): 591-604.
[Cao Y T,Liu C L,Yan H,Jiao P C,Zhang H,Lü F L,Ding T.2016. Research on evaporite deposit and its controlling factors for saline lake chain of Tarim Basin and Central Asia Basin during Mesozoic-Cenozoic period. Mineral Deposits, 35(3): 591-604]
[3] 陈荣林. 1996. 塔里木盆地第三纪含盐系地质特征研究. 化工矿产地质, 18(4): 276-283.
[Chen R L.1996. Geological characteristics of the tertiary salt-bearing sequences in Tarim Basin. Geology of Chemical Minerals, 18(4): 276-283]
[4] 丁道桂,刘伟新,崔可锐,王道轩,孙世群. 1997. 塔里木中新生代前陆盆地构造分析与油气领域. 石油实验地质, 19(2): 97-107.
[Ding D G,Liu W X,Cui K R,Wang D X,Sun S Q.1997. Tectonic analyses and hydrocarbon domains in the Mesozoic and Cenozoic foreland basins of Tarim. Petroleum Geology & Experiment, 19(2): 97-107]
[5] 冯展涛. 2022. 青藏高原东北缘临夏盆地始新世地层序列及其构造—气候意义. 兰州大学博士学位论文.
[Feng Z T.2022. Eocene stratigraphic sequence and its tectonic-climatic significance in Linxia Basin,northeastern margin of Qinghai-Tibet Plateau. Doctoral dissertation of Lanzhou University]
[6] 郭宪璞. 1991. 新疆克孜勒苏群的沉积环境探讨: 兼论塔里木盆地西部白垩系最低海相层位. 地质学报, 65(2): 188-198.
[Guo X P.1991. An approach to the depositional environment of the Cretaceous Kizilsu group: the lowermost marine horizon of the Cretaceous in the western Tarim Basin. Acta Geologica Sinica, 65(2): 188-198]
[7] 郭宪璞,丁孝忠,何希贤,李汉敏,苏新,彭阳. 2002. 塔里木盆地中新生代海侵和海相地层研究的新进展. 地质学报, 76(3): 299-307.
[Guo X P,Ding X Z,He X X,Li H M,Su X,Peng Y.2002. New progress in the study of marine transgressional events and marine strata of the meso-cenozoic in the Tarim Basin. Acta Geologica Sinica, 76(3): 299-307]
[8] 何承全,宋之琛,祝幼华. 2009. 中国沟鞭藻类化石. 北京: 科学出版社.
[He C Q,Song Z C,Zhu Y H.2009. China Dinoflagellate Fossils. Beijing: Science Press]
[9] 何登发,贾承造,德生,张朝军,孟庆任,石昕. 2005. 塔里木多旋回叠合盆地的形成与演化. 石油与天然气地质, 26(1): 64-77.
[He D F,Jia C Z,De S,Zhang C J,Meng Q R,Shi X.2005. Formation and evolution of polycyclic superimposed Tarim Basin. Oil & Gas Geology, 26(1): 64-77]
[10] 胡兰英. 1982. 塔里木盆地晚第三纪有孔虫古生态及地质意义. 科学通报, 27(15): 938-941.
[Hu L Y.1982. Late Tertiary foraminifer ecology of the Tarim Basin and its geological significance. Chinese Science Bulletin, 27(15): 938-941]
[11] 郇志鹏,胡剑风,王志民,宋金鹏,莫涛,郝祥保,田盼盼,崔德育,杨敬博,李浩平,刘新宇,平忠伟. 2022. 库车坳陷古近系盐底卡层技术研究与应用. 中国石油勘探, 27(1): 142-150.
[Huan Z P,Hu J F,Wang Z M,Song J P,Mo T,Hao X B,Tian P P,Cui D Y,Yang J B,Li H P,Liu X Y,Ping Z W.2022. Research and application of the base salt rock discrimination of the Paleogene in Kuqa Depression. China Petroleum Exploration, 27(1): 142-150]
[12] 贾承造. 1997. 中国塔里木盆地构造特征与油气. 北京: 石油工业出版社.
[Jia C Z.1997. Structural Characteristics and Oil and Gas in Tarim Basin,China. Beijing: Petroleum Industry Press]
[13] 贾承造. 1999. 塔里木盆地构造特征与油气聚集规律. 新疆石油地质, 20(3): 177-183.
[Jia C Z.1999. Structural characteristics and oil/gas accumulative regularity in Tarim Basin. Xinjiang Petroleum Geology, 20(3): 177-183]
[14] 贾进华. 2002. 新疆库车坳陷中、新生界碳酸盐岩及其成因意义. 古地理学报, 4(4): 30-38.
[Jia J H.2002. Carbonate rocks and their genetic significance of the Mesozoic and Cenozoic in kuqa depression of Xinjiang area. Journal of Palaeogeography(Chinese Edition), 4(4): 30-38]
[15] 李玉英. 2007. 库车盆地古近纪沉积环境与岩相古地理研究. 中国地质大学(北京)硕士学位论文.
[Li Y Y.2007. The research on depositional environments and lithofacies palaeogeography in Kuqa Basin. Masteral dissertation of China University of Geosciences(Beijing)]
[16] 刘成林,王弭力,焦鹏程,陈永志. 2006. 世界主要古代钾盐找矿实践与中国找钾对策. 化工矿产地质, 28(1): 1-8.
[Liu C L,Wang M L,Jiao P C,Chen Y Z.2006. The exploration experiences of potash deposits in the world and probing of countermeasures of China's future potash-deposits investigation. Geology of Chemical Minerals, 28(1): 1-8]
[17] 刘成林,曹养同,杨海军,焦鹏程,顾乔元. 2013a. 库车前陆盆地古近纪—新近纪盐湖环境变迁及其成钾效应探讨. 地球学报, 34(5): 547-558.
[Liu C L,Cao Y T,Yang H J,Jiao P C,Gu Q Y.2013a. Discussion on paleogene-neogene Environmental Change of Salt Lakes in Kuqa Foreland Basin and its potash-forming Effect. Acta Geoscientica Sinica, 34(5): 547-558]
[18] 刘成林,焦鹏程,宣之强,曹养同,赵宪福. 2013b. 库车盆地古近系蒸发岩中钾盐矿物研究进展. 地质论评, 59(2): 233-234.
[Liu C L,Jiao P C,Xuan Z Q,Cao Y T,Zhao X F.2013b. Research progress of sylvite in the Paleogene Evaporates in Kuqa Basin. Geological Review, 59(2): 233-234]
[19] 刘子涵,李建明,陈琰,柳金城,崔俊. 2022. 微量元素在沉积环境中的应用: 以柴西英西地区下干柴沟组上段为例. 中外能源, 27(6): 23-34.
[Liu Z H,Li J M,Chen Y,Liu J C,Cui J.2022. Application of trace elements in sedimentary environment: case study of upper member of lower Ganchaigou formation in Yingxi area,Western Qaidam Basin. Sino-Global Energy, 27(6): 23-34]
[20] 卢华复,陈楚铭,刘志宏,贾东,王国强,贾承造. 2000. 库车再生前陆逆冲带的构造特征与成因. 石油学报, 21(3): 18-24.
[Lu H F,Chen C M,Liu Z H,Jia D,Wang G Q,Jia C Z.2000. The structural features and origin of the kuqa rejuvenation foreland thrust belt. Acta Petrolei Sinica, 21(3): 18-24]
[21] 马宝林,王琪. 1997. 青海湖现代沉积物的元素分布特征. 沉积学报, 15(3): 120-125.
[Ma B L,Wang Q.1997. Distribution characteristics of elements in modern sediments of Qinghai Lake. Acta Sedimentologica Sinica, 15(3): 120-125]
[22] 马新华. 2000. 含盐油气盆地. 北京: 石油工业出版社.
[Ma X H.2000. Saline Oil and Gas Basin. Beijing: Petroleum Industry Press]
[23] 苗运法,方小敏,宋之琛,吴福莉,韩文霞. 2008. 青藏高原北部始新世孢粉记录与古环境变化. 中国科学(D辑),(2): 187-196.
[Miao Y F,Fang X M,Song Z C,Wu F L,Han W X.2008. Eocene palynological records and paleo-environmental changes in the northern Tibetan Plateau. Science in China Press(Series D),(2): 187-196]
[24] 邵龙义,何志平,顾家裕,罗文林,贾进华,刘永福,张丽娟,张鹏飞. 2006. 塔里木盆地古近纪岩相古地理. 古地理学报, 8(3): 353-364.
[Shao L Y,He Z P,Gu J Y,Luo W L,Jia J H,Liu Y F,Zhang L J,Zhang P F.2006. Lithofacies palaeogeography of the Paleogene in Tarim Basin. Journal of Palaeogeography(Chinese Edition), 8(3): 353-364]
[25] 宋金鹏,田盼盼,代俊杰,杨连刚,戴瑞瑞,郭喜阳. 2021. 塔里木盆地库车坳陷膏盐岩分布特征及油气地质意义. 断块油气田, 28(6): 800-804.
[Song J P,Tian P P,Dai J J,Yang L G,Dai R R,Guo X Y.2021. Distribution characteristics of gypsum-salt rock and petroleum geological significance in Kuqa Depression of Tarim Basin. Fault-Block Oil & Gas Field, 28(6): 800-804]
[26] 苏新,郭宪璞,丁孝忠. 2003. 塔里木北部库车前陆盆地晚白垩世和古新世的钙质超微化石组合. 现代地质, 17(4): 370-377.
[Su X,Guo X P,Ding X Z.2003. Late Cretaceous and Paleocene calcareous nannofossil assemblages from Kuqa foreland Basin in the northern Tarim Basin. Geoscience, 17(4): 370-377]
[27] 孙宏伟. 2014. 新疆莎车盆地上白垩统—古近系蒸发岩沉积特征及其找钾指示意义. 中国地质大学(北京)硕士学位论文.
[Sun H W.2014. Sedimentary characteristics of Upper Cretaceous-Paleogene evaporite in Shache Basin,Xinjiang and its indicative significance for potassium prospecting. Masteral dissertation of China University of Geosciences]
[28] 谭红兵,于升松. 1999. 我国湖泊沉积环境演变研究中元素地球化学的应用现状及发展方向. 盐湖研究, 7(3): 58-65.
[Tan H B,Yu S S.1999. Present situation and future development of elemental geochemistry in the study of lake sediments' evolution. Journal of Salt Lake Research, 7(3): 58-65]
[29] 谭红兵,马海州,许建新,肖应凯,王建国,李廷伟. 2005. 塔里木盆地西部古盐岩同位素地球化学与成钾预测研究. 地球学报,26(B09): 174-179.
[Tan H B,Ma H Z,Xu J X,Xiao Y K,Wang J G,Li T W.2005. Isotope geochemistry of ancient salt rocks and prognosis of sylvinite deposits in western Tarim Basin. Acta Geoscientica Sinica,26(B09): 174-179]
[30] 唐天福. 1989. 新疆塔里木盆地西部白垩纪至早第三纪海相地层及含油性. 北京: 科学出版社.
[Tang T F.1989. Cretaceous-Paleogene Marine Strata and Oil-bearing in Western Tarim Basin,Xinjiang. Beijing: Science Press]
[31] 田军,杨海军,吴超,莫涛,朱文慧,史玲玲. 2020. 博孜9井的发现与塔里木盆地超深层天然气勘探潜力. 天然气工业, 40(1): 11-19.
[Tian J,Yang H J,Wu C,Mo T,Zhu W H,Shi L L.2020. Discovery of Well Bozi 9 and ultra-deep natural gas exploration potential in the Kelasu tectonic zone of the Tarim Basin. Natural Gas Industry, 40(1): 11-19]
[32] 王得林. 2000. 新疆古近纪和新近纪古地理. 新疆地质, 18(4): 352-356.
[Wang D L.2000. Palaeogeography of the Paleoneogone in Xinjiang. Xinjiang Geology, 18(4): 352-356]
[33] 王凡,邓小林,郑绵平,韦钊,王淑丽,赵玉海,刘星旺,王占文. 2022. 新疆库车坳陷西段膏盐层沉积、地球化学特征及找钾方向. 地球科学,47(1): 56-71.
[Wang F,Deng X L,Zheng M P,Wei Z,Wang S L,Zhao Y H,Liu X W,Wang Z W.2022. Sedimentary-geochemical characteristics and potash-prospecting potential of gypsum-salt layer in western Kuqa Depression. Earth Science,47(1): 56-71]
[34] 王淑丽,郑绵平,王永明,王凡,王英林,张震,吴静依,李洪普. 2019. 中国盐湖地球化学发展历程与研究进展. 科学技术与工程, 19(9): 1-9.
[Wang S L,Zheng M P,Wang Y M,Wang F,Wang Y L,Zhang Z,Wu J Y,Li H P.2019. Advances and development history of geochemistry on salt lakes in China. Science Technology and Engineering, 19(9): 1-9]
[35] 王兴元,尹宏伟,邓小林,韦钊. 2015. 库车坳陷新生代盐岩锶同位素特征及物质来源分析. 南京大学学报(自然科学), 51(5): 1068-1074.
[Wang X Y,Yin H W,Deng X L,Wei Z.2015. Strontium isotope characteristics and the origin of Cenozoic salt deposits in Kuqa Depression. Journal of Nanjing University(Natural Science), 51(5): 1068-1074]
[36] 王招明. 2004. 库车前陆盆地露头区油气地质. 北京: 石油工业出版社.
[Wang Z M.2004. Petroleum Geology in Outcrop Area of Kuqa Foreland Basin. Beijing: Petroleum Industry Press]
[37] 王招明,谢会文,李勇,雷刚林,吴超,杨宪彰,马玉杰,能源. 2013. 库车前陆冲断带深层盐下大气田的勘探和发现. 中国石油勘探, 18(3): 1-11.
[Wang Z M,Xie H W,Li Y,Lei G L,Wu C,Yang X Z,Ma Y J,Neng Y.2013. Exploration and discovery of large and deep subsalt gas fields in kuqa foreland thrust belt. China Petroleum Exploration, 18(3): 1-11]
[38] 许丽,李江海,王洪浩,黄少英,能源. 2016. 库车坳陷大北地区古近纪沉积特征及盐湖演化. 特种油气藏, 23(5): 56-61.
[Xu L,Li J H,Wang H H,Huang S Y,Neng Y.2016. Paleogene sedimentary properties and salt lake evolution in Dabei of Kuqa Depression. Special Oil & Gas Reservoirs, 23(5): 56-61]
[39] 徐洋,曹养同,刘成林,焦鹏程. 2018. 库车盆地始新世盐湖物源及蒸发浓缩程度研究. 地质学报, 92(8): 1617-1629.
[Xu Y,Cao Y T,Liu C L,Jiao P C.2018. Provenance and degree of evaporation and concentration of Eocene salt lake in the Kuqa Basin. Acta Geologica Sinica, 92(8): 1617-1629]
[40] 徐洋,刘成林,曹养同. 2021. 新疆库车盆地中始新世成盐演化特征: 以KL4钻孔为例. 地质学报, 95(7): 2183-2192.
[Xu Y,Liu C L,Cao Y T.2021. Salt-forming evolution characteristics of Middle Eocene in the Kuqa Basin,Xinjiang: A case study of borehole KL4. Acta Geologica Sinica, 95(7): 2183-2192]
[41] 雍天寿,单金榜. 1986. 白垩纪及早第三纪塔里木海湾的形成与发展. 沉积学报, 04(3): 67-75.
[Yong T S,Shan J B.1986. The development and formation in the Tarim Bay in Cretaceous-Paleogene ages. Acta Sedimentologica Sinica, 04(3): 67-75]
[42] 岳乐平,邱占祥,颉光普,邱铸鼎,张莉,张云翔,Heller F.2003. 兰州盆地永登剖面记录的第三纪沉积环境. 沉积学报, 21(4): 683-687.
[Yue L P,Qiu Z X,Xie G P,Qiu Z D,Zhang L,Zhang Y X,F H.2003. Sedimentary environment of Tertiary recorded in the Yongdeng section of Lanzhou Basin. Acta Sedimentologica Sinica, 21(4): 683-687]
[43] 张朝军,田在艺. 1998. 塔里木盆地库车坳陷第三系盐构造与油气. 石油学报, 19(1): 6-10.
[Zhang C J,Tian Z Y.1998. Tertiary salt structures and hydrocarbons in Kuqa Depression of Tarim Basin. Acta Petrolei Sinica, 19(1): 6-10]
[44] 张华,刘成林,曹养同,孙宏伟,王立成. 2013. 塔里木古海湾新生代海退时限及方式的初步探讨. 地球学报, 34(5): 577-584.
[Zhang H,Liu C L,Cao Y T,Sun H W,Wang L C.2013. A tentative discussion on the time and the way of marine regression from Tarim Bay during the Cenozoic. Acta Geoscientica Sinica, 34(5): 577-584]
[45] 张涛. 2014. 天山南麓库车坳陷新生代高精度磁性地层与构造演化. 兰州大学博士学位论文.
[Zhang T.2014. Cenozoic high-precision magnetic strata and tectonic evolution in Kuqa Depression at the southern foot of Tianshan Mountains. Doctoral dissertation of Lanzhou University]
[46] 张勇刚,吕福亮,范国章,王彬,李丽,李东,邵大力,杨姣. 2012. 盐相关盆地油气地质特征及其勘探认识: 以红海盆地为例. 盐湖研究, 20(1): 9-15.
[Zhang Y G,Lü F L,Fan G Z,Wang B,Li L,Li D,Shao D L,Yang J.2012. Salt-related basin hydrocarbon geology characteristics and exploration recognition: a case study of Red Sea basin. Journal of Salt Lake Research, 20(1): 9-15]
[47] 张一勇. 1995. 中国早第三纪孢粉植物群纲要. 古生物学报, 34(2): 212-227.
[Zhang Y Y.1995. Outline of palaeogene palynofloras of China. Acta Palaeontologica Sinica, 34(2): 212-227]
[48] 张一勇,詹家祯. 1991. 新疆塔里木盆地西部晚白垩世至早第三纪孢粉. 北京: 科学出版社.
[Zhang Y Y,Zhan J Z. 1991. Sporopollen from Late Cretaceous to Early Tertiary in Western Tarim Basin,Xinjiang. Beijing: Science Press]
[49] 章振国,高继雷,张向文. 2010. 塔里木盆地古代蒸发岩硫同位素地球化学研究. 甘肃地质, 19(1): 32-37.
[Zhang Z G,Gao J L,Zhang X W.2010. Geochemistry of sulfur isotope of paleo-evaporites in Tarim Basin. Gansu Geology, 19(1): 32-37]
[50] 张志亮,沈忠悦,汪新,唐鹏程,余养里,赵博,潘小青,石林权. 2013. 库车坳陷克拉苏河新生代沉积岩磁组构特征与古流向分析. 地球物理学报, 56(2): 567-578.
[Zhang Z L,Shen Z Y,Wang X,Tang P C,Yu Y L,Zhao B,Pan X Q,Shi L Q.2013. Characteristics of magnetic fabrics and paleocurrent directions of Cenozoic sediments in the Kelasu River,Kuqa Depression. Chinese Journal of Geophysics, 56(2): 567-578]
[51] 郑民,孟自芳. 2006. 新疆拜城古近系磁性地层划分. 沉积学报,(5): 650-656.
[Zheng M,Meng Z F.2006. Magnetostratigraphy of tertiary system in Baicheng,Xinjiang. Acta Sedimentologica Sinica, 24(5): 650-656]
[52] 郑绵平,袁鹤然,张永生,刘喜方,陈文西,李金锁. 2010. 中国钾盐区域分布与找钾远景. 地质学报, 84(11): 1523-1553.
[Zheng M P,Yuan H R,Zhang Y S,Liu X F,Chen W X,Li J S.2010. Regional distribution and prospects of potash in China. Acta Geologica Sinica, 84(11): 1523-1553]
[53] 钟逸斯,王立成,董浩伟. 2022. 蒸发岩沉积特征及环境综述. 沉积学报, 40(5): 1188-1214.
[Zhong Y S,Wang L C,Dong H W.2022. Evaporite sedimentary characteristics and environment: a review. Acta Sedimentologica Sinica, 40(5): 1188-1214]
[54] 祝幼华,赵媛媛,钟石兰. 2012. 塔里木盆地库车坳陷小库孜拜剖面古近纪钙质超微化石. 古生物学报, 51(3): 328-333.
[Zhu Y H,Zhao Y Y,Zhong S L.2012. Palaeogene calcareous nannofossils from the Xiaokuzibai section of the Kuqa Depression,Tarim Basin. Acta Palaeontologica Sinica, 51(3): 328-333]
[55] 卓勤功,李勇,宋岩,杨宪彰,赵孟军,方世虎,柳少波,鲁雪松. 2013. 塔里木盆地库车坳陷克拉苏构造带古近系膏盐岩盖层演化与圈闭有效性. 石油实验地质, 35(1): 42-47.
[Zhuo Q G,Li Y,Song Y,Yang X Z,Zhao M J,Fang S H,Liu S B,Lu X S.2013. Evolution of Paleogene saline deposits and effectiveness of traps in Kelasu tectonic zone,Kuqa Depression,Tarim Basin. Petroleum Geology & Experiment, 35(1): 42-47]
[56] Fan X J,Lu Y C,Zhang J Y,Wu S Q,Zhang L A,Du X J,Cui Q Y,Wang H.2022. Lithofacies characteristics,depositional environment and sequence stratigraphic framework in the saline lacustrine basin: a case study of the Eocene low member of Xingouzui Formation,Jianghan Basin,China. Energies, 15: 6235.
[57] Fang X M,Fang Y H,Zan J B,Zhang W L,Song C H,Appel E,Meng Q Q,Miao Y F,Dai S,Lu Y,Zhang T.2019. Cenozoic magnetostratigraphy of the Xining Basin,NE Tibetan Plateau,and its constraints on paleontological,sedimentological and tectonomorphological evolution. Earth-Science Reviews, 190: 460-485.
[58] Hardie L,Smoot J,Eugster H.1978. Saline Lakes and their deposits: A sedimentological approach. Modern and ancient lake sediments,7-41.
[59] Hyland E G,Huntington K W,Sheldon N D,Reichgelt T.2018. Temperature seasonality in the North American continental interior during the Early Eocene Climatic Optimum. Climate of the Past, 14: 1391-1404.
[60] Lauretano V,Littler K,Polling M,Zachos J C,Lourens L J.2015. Frequency,magnitude and character of hyperthermal events at the onset of the Early Eocene climatic optimum. Clim Past, 11: 1313-1324.
[61] Miller K G,Browning J V,Schmelz W J,Kopp R E,Mountain G S,Wright J D.2020. Cenozoic Sea-level and cryospheric evolution from deep-sea geochemical and continental margin records. Science Advances, 6: eaaz1346.
[62] Qin P,Zhong D K,Su C,Yang X Z,Sun H T,Zhang H,Song L,Yang Y,Wang H X.2023. A unique saline lake sequence in the eastern Tethyan Ocean in responses to the Palaeocene-Eocene thermal maximum: a case study in the Kuqa Depression,Tarim Basin,NW China. Journal of Asian Earth Sciences, 250: 105594.
[63] Van Dijk J,Fernandez A,Bernasconi S M,Caves Rugenstein J K,Passey S R,White T.2020. Spatial pattern of super-greenhouse warmth controlled by elevated specific humidity. Nature Geoscience, 13: 739-744.
[64] Warren J.2016. Evaporites: a Geological Compendium. Springer: 408-413.
[65] Westerhold T,Röhl U,Donner B,Zachos J C.2018. Global extent of early Eocene hyperthermal events: a new Pacific benthic foraminiferal isotope record from shatsky rise(ODP site 1209). Paleoceanog and Paleoclimatol, 33: 626-642.
[66] Xu Y,Cao Y T,Liu C L,Zhang H,Nie X.2020. The history of transgressions during the Late Paleocene-Early Eocene in the Kuqa depression,Tarim Basin: Constraints from C-O-S-Sr isotopic geochemistry. Minerals, 10: 834.
[67] Zachos J,Pagani M,Sloan L,Thomas E,Billups K.2001. Trends,Rhythms,and Aberrations in Global Climate 65 Ma to Present. Science, 292: 686-693.
[68] Zachos C,Dickens R,Zeebe E.2008. An Early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics. Nature, 451: 279-283.
[69] Zhang Z L,Shen Z Y,Sun J M,Wang X,Tian Z H,Pan X Q,Shi L Q.2015. Magnetostratigraphy of the Kelasu section in the Baicheng Depression,Southern Tian Shan,Northwestern China. Journal of Asian Earth Sciences, 111: 492-504.
[70] Zuo X C,Li C L,Zhang J L,Ma G Y,Chen P P.2020. Geochemical characteristics and depositional environment of the Shahejie Formation in the Binnan Oilfield,China. Journal of Geophysics and Engineering, 17: 539-551.

选择文件类型/文献管理软件名称

选择包含的内容

早始新世温室气候与海侵作用对库车坳陷库姆格列木群含盐层系沉积的协同控制作用^*

Collaborative controls of the Early-Eocene greenhouse climates and transgression on deposition of salt-bearing sequence of Kumugeliemu Group in Kuqa Depression

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]	刘大卫, 李映涛, 韩俊, 张继标, 汝智星, 杨孝群, 王石, 黄诚, 肖重阳. 塔里木盆地顺北地区奥陶系鹰山组超深层白云岩类型及成储潜力评价^*[J]. 古地理学报, 2025, 27(1): 126-140.
[2]	贾进华. 塔里木盆地阿瓦提凹陷三叠系层序特征与沉积古地理演化^*[J]. 古地理学报, 2024, 26(4): 763-778.
[3]	胡宗全, 高志前, 刘旺威, 卫端. 塔里木盆地东北缘兴地断裂以北地区下寒武统富有机质泥页岩沉积环境与发育机制^*[J]. 古地理学报, 2023, 25(6): 1235-1256.
[4]	陈海颖, 张立强. 基于成岩相的深层碎屑岩优质储集层发育规律研究: 以塔里木盆地顺9井区柯坪塔格组为例[J]. 古地理学报, 2023, 25(6): 1379-1393.
[5]	操应长, 梁超, 韩豫, 葸克来, 王俊然, 籍士超, 梅俊芳. 基于物质来源及成因的细粒沉积岩分类方案探讨^*[J]. 古地理学报, 2023, 25(4): 729-741.
[6]	王珊, 曹颖辉, 闫磊, 杜德道, 马德波, 张翔, 陈志勇, 周慧, 杨敏, 白莹. 塔里木盆地中下寒武统蒸发岩沉积特征及发育模式^*[J]. 古地理学报, 2023, 25(4): 889-905.
[7]	钱一雄, 何治亮, 陈代钊, 储呈林, 董少峰, 张庆珍. 塔北埃迪卡拉系奇格布拉克组多类型共生鲕粒特征及其成因探讨^*[J]. 古地理学报, 2023, 25(1): 56-74.
[8]	贾润幸, 方维萱. 塔里木盆地西南部下白垩统克孜勒苏群沉积特征与成矿成藏作用^*[J]. 古地理学报, 2022, 24(5): 1017-1028.
[9]	韩强, 耿锋, 虎北辰, 高山林, 金仙梅, 王玺童, 李振宇. 塔里木盆地中石化探区含氦气藏资源调查研究^*[J]. 古地理学报, 2022, 24(5): 1029-1036.
[10]	赖锦, 包萌, 刘士琛, 李栋, 王松, 杨科夫, 陈旭, 王贵文, 丁修建. 塔里木盆地深层、超深层白云岩优质储集层测井预测^*[J]. 古地理学报, 2021, 23(6): 1225-1242.
[11]	郑剑锋, 刘禹, 朱永进, 梁峰. 塔里木盆地乌什地区上震旦统奇格布拉克组地球化学特征及其地质意义^*[J]. 古地理学报, 2021, 23(5): 983-998.
[12]	刘学飞, 王庆飞, 马遥, 李中明, 赵利华, 周智慧, 刘百顺, 马欣莉. 华北克拉通南缘石炭系本溪组铁-铝黏土矿物质来源: 以河南三门峡大安铝黏土矿床为例^*[J]. 古地理学报, 2020, 22(5): 965-976.
[13]	鲍志东, 季汉成, 梁婷, 韦明洋, 史燕青, 李宗峰, 鲁锴, 向鹏飞, 张华, 严睿, 郭玉鑫, 李卓伦, 万谱, 杨志波, 麻晓东, 刘锐, 刘灿星, 钟旭临, 郭晓琦, 蔡忠贤, 张水昌. 中新元古界原生白云岩: 以中国典型台地区为例^*[J]. 古地理学报, 2019, 21(6): 869-884.
[14]	郑剑锋, 袁文芳, 黄理力, 潘文庆, 乔占峰, 杨果. 塔里木盆地肖尔布拉克露头区下寒武统肖尔布拉克组沉积相模式及其勘探意义^*[J]. 古地理学报, 2019, 21(4): 589-602.
[15]	贾进华, 张立平, 陈秀艳. 塔里木盆地乌什凹陷西部石炭系—二叠系沉积演化^*[J]. 古地理学报, 2018, 20(3): 423-434.

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

早始新世温室气候与海侵作用对库车坳陷库姆格列木群含盐层系沉积的协同控制作用*

Collaborative controls of the Early-Eocene greenhouse climates and transgression on deposition of salt-bearing sequence of Kumugeliemu Group in Kuqa Depression

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

早始新世温室气候与海侵作用对库车坳陷库姆格列木群含盐层系沉积的协同控制作用^*