Sequence stratigraphy and sedimentary filling evolution of the Cretaceous in Southwest Depression,Tarim Basin
Received date: 2016-12-21
Revised date: 2017-07-27
Online published: 2017-09-10
Based on the comprehensive correlation of outcrops data,logging data and drilling data,we established the Cretaceous sequence stratigraphic framework in the piedmont zone of the south Tianshan and western Kunlun mountains in Southwest Depression,Tarim Basin.According to the regional unconformities and regional mutations in the interface of sedimentary facies,two second-order sequences of the Cretaceous in the study area were recognized,which can be further divided into four third-order sequences based on the change of sedimentary facies,transforming surface of stratigraphic accumulation type and the structure of sedimentary cycle.Based on the analysis from outcrops and wireline logging datasets in the study area,we recognized five sedimentary facies including alluvial fan,braided river,meandering river,braided river delta,meandering river delta.The distribution pattern of sedimentary systems for each sequence is systematically studied,through which the spatial distribution and vertical evolution of depositional systems are revealed.Studies show that the deposition scope and the depositional systems had changed significantly in Cretaceous in Southwest Depression.The large-scale sea transgression events were generally proved by the evidence that the sedimentary scope changed from piedmont belt to intra-basin in the study area.The sedimentary systems showed an overall evolution process from continental sedimentation to marine deposition.
Ren Yu-ze,Lin Chang-song,Gao Zhi-yong,Liu Jing-yan,Song Ning-ning . Sequence stratigraphy and sedimentary filling evolution of the Cretaceous in Southwest Depression,Tarim Basin[J]. Natural Gas Geoscience, 2017 , 28(9) : 1298 -1311 . DOI: 10.11764/j.issn.1672-1926.2017.08.002
[1]Jia Chengzao.The structures of basin and range system around the tibetan plateau and the distribution of oil and gas in the Tarim Basin[J].Geotectonica et Metallogenia,2009,33(1):1-9.[贾承造.环青藏高原巨型盆山体系构造与塔里木盆地油气分布规律[J].大地构造与成矿学,2009,33(1):1-9.]
[2]Lin Changsong,Sequenceand depositional architecture of sedimentary basin and process responses[J].Acta Sedimentologica Sinica,2009,27(5):849-862.[林畅松.沉积盆地的层序和沉积充填结构及过程响应[J].沉积学报,2009,27(5):849-862.]
[3]Liu Jiaduo,Wang Jun,Wang Yibin,et al.Sequence-lithology Palaeogeography charateristic of Cretaceous in northern Kashi area of Tarim Basin[J].Journal of Earth Sciences and Environment,2013,35(1):1-14.[刘家铎,王峻,王易斌,等.塔里木盆地喀什北地区白垩系层序—岩相古地理特征[J].地球科学与环境学报,2013,35(1):1-14.]
[4]Zheng Qiufeng.The Character of Cretaceous Sequence Stratigraphy and Depositional System in Northern Kashgar,Tarim Basin[D].Chengdu:Chengdu University of Technology,2012.[郑秋枫.塔里木盆地喀什北地区白垩系层序地层及沉积体系特征[D].成都:成都理工大学,2012.]
[5]Ding Xiaozhong.The Sequence Stratigraphic Response to the Basin Orogene Coupling Process of Cretaceous-Tertiary in Tarim Basin,China[D].Beijing:China University of Geosciences,2003.[丁孝忠.塔里木盆地白垩纪—第三纪盆山耦合过程的层序地层响应[D].北京:中国地质大学,2003.]
[6]Zhuang Honghong,Guo Feng,Zhou Xue.Evolution of sedimentary environment in Late Cretaceous,Kunlun Mountain Front,Tarim Basin[J].Journal of Xi’an University of Science and Technology,2013,33(1):39-45.[ 庄红红,郭峰,周雪.塔西南昆仑山前地区晚白垩世沉积演化[J].西安科技大学学报,2013,33(1):39-45.]
[7]Ma Donghua,Yang Zijiang,et al.Evolution of the Cenozoic in southwestern Tarim Basin[J].Xinjiang Geology,2003,21(1):92-95.[马东华,杨子江.塔里木盆地西南新生代盆地演化特征[J].新疆地质,2003,21(1):92-95.]
[8]Zhang Wei,Qi Jiafu,Lei Ganglin,et al.Deformation model of contraction structure of west Kunlun piedmont thrust belt in southwestern depression of Tarim Basin[J].Xinjiang Petroleum Geology,2010,31(6):567-571.[张玮,漆家福,雷刚林.塔西南坳陷西昆仑山前冲断带的收缩构造变形模式[J].新疆石油地质,2010,31(6):567-571.]
[9]Liu Yufan,Chen Honghan,Tang Daqing,et al.Division of Mesozoic and Cenozoicstructural units in Tarim Basin[J].Geological Science and Techno-logy Information,2012,31(3):24-30.[刘凡瑀,陈红汉,唐大卿,等.塔里木盆地中—新生界构造单元划分[J].地质科技情报,2012,31(3):24-30.]
[10]Catuneanu O.Principles of Sequence Stratigraphy[M].Amsterdam:Elsevier Science,2006,1-375.
[11]Vail P R,Gerald R B.Sequene Stratigraphic Concepts Applied to Paleogene Outcrops,Gulf and Atlantic,Sea-level Changes:An Integrated Approach[C].SPEM Special Publication,1988,42:309-328.
[12]Li Meng,Zhang Shiben,Tan Zejin,et al.The Classification and Correlation of Strata and Palaeoenvironment Study the Cretaceous,in Southwestern Tarim Basin[R].Korla:Tarim Oilfield Branch,2003.[李猛,张师本,谭泽金,等.塔里木油气白垩系划分对比及古环境研究[R].库尔勒:塔里木油田分公司,2003.]
[13]Shi Jian,Xiao Lixin,Mou Zonghai,et al.The Study of Strata,Sedimentary and Reservoir in Southwestern Tarim Basin[R].Korla:Tarim Oilfield Branch,1998.[史基安,肖立新,牟忠海,等.塔西南地区地层、沉积及储层研究[R].库尔勒:塔里木油田分公司,1998.]
[14]Zhang Yingzhi,Lin Changsong,Gao Zhiyong.Depositonal paleogeography and provenance analysis of Early Cretaceous Southwest Depression of Tarim Basin[J].Geoscience,2014,28(4):791-798.[张英志,林畅松,高志勇,等.塔西南坳陷早白垩世物源体系和沉积古地理分析[J].现代地质,2014,28(4):791-798.]
[15]Soble E R.Basin analysis of the Jurassic-Lower Cretaceous southwest Tarim Basin,northwest China[J].Geological Society of America Bulletin,1999,111(5):709-724.
[16]Fang Aimin,Ma Jianying,Wang Shigang,et al.Sedimentary tectonic evolution of the southwestern Tarim Basin and west Kunlun orogen since Late Paleozoic[J].Acta Petrologica Sinica,2009,25(12):3396-3406.[方爱民,马建英,王世刚,等.西昆仑—塔西南坳陷晚古生代以来的沉积构造演化[J].岩石学报,2009,25(12):3396-3406.]
[17]Wang Yong,Fu Derong.The Sedimentary-Tectonicevolution of the Southwest Tarim Basin from Crataceous to Paleogene[J].Acta Geoscientia Sinica,1996,17(1):32-40.[王永,傅德荣.塔里木盆地西南部白垩纪一早第三纪沉积构造演化[J].地球学报,1996,17(1):32-40.]
[18]Yang Haijun,Wang Jianpo,Li Meng,et al.Lithofacies and depositional environments of the Kalataer Formation,Paleogene,Southwest Tarim Basin[J].Journal of Stratigraphy,2011,35(2):129-138.[杨海军,王建坡,李猛,等.塔西南古近系卡拉塔尔组岩相特征与沉积环境[J].地层学杂志,2011,35(2):129-137.]
[19]Yang Haijun,Shen Jianwei,Zhang Lijuan,et al.Serpulids and their paleoecology of the Paleogene Kalatar Formation in southwest Tarim Basin of China[J].Science China:Earth Sciences,2012,42(11):1634-1646.[杨海军,沈建伟,张丽娟,等.塔里木盆地西南地区古近系卡拉塔尔组龙介类化石及其古生态[J].中国科学:地球科学,2012,42(11):1634-1646.]
[20]Zhang Huiliang,Shen Yang,Tu Xiaolong,et al.The carbonate depositional features of Yigeziya Formation of Upper Cretaceous in Tarim Basin and their geological implication[J].Acta Sedimentologica Sinica,2002,20(4):600-607.[张惠良,沈扬,屠小龙,等.塔里木盆地上白垩统依格孜牙组碳酸盐沉积学特征及地质意义[J].沉积学报,2002,20(4):600-607.]
[21]Liao Lin,Cheng Xiaogan,Wang Buqing,et al.Reconstruction of Mesozoic sedimentary paleoenvironment in the southwestern Tarim Basin,Northwestern China[J].Acta Geologica Sinica,2010,84(8):1195-1207.[廖林,程晓敢,王步清,等.塔里木盆地西南缘中生代沉积古环境恢复[J].地质学报,2010,84(8):1195-1207.]
[22]Ding Xiaozhong,Liu Xun,Wu Shaozu,et al.Discussion on the Cretaceous-Plaeogene sedimentary features and environments of Kuzgongsu area,western Tarim Basin[J].Xinjiang Geology,1993,11(3):179-193 .[丁孝忠,刘训,吴绍祖,等.塔里木盆地西部库孜贡苏地区白垩—早第三纪沉积特征及沉积环境探讨[J].新疆地质,1993,11(3):179-193.]
[23]Jia Jinhua.Sedimentary characteristics and Palaeogeography of the Early Cretaceous in Tarim Basin[J].Journal of Palaeogeography,2009,11(2):167-176.[贾进华.塔里木盆地早白垩世沉积相特征与古地理[J].古地理学报,2009,11(2):167-176.]
[24]Yong Tianshou,Shan Jinbang.The development and formation in the Tarim Bay in Cretaceous-Paleogene ages[J].Acta Sedimentologica Sinica,1986,4(3):67-75.[雍天寿,单金榜.白垩纪及早第三纪塔里木海湾的形成与发展[J].沉积学报,1986,4(3):67-75.]
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