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学科主题: Geology ; Paleontology
题名: Mixed carbonate-clastic facies in the Eocene Kalatar Formation of the southwest Tarim Basin (NW China): tectonic and climatic controls
作者: Yang, HQ ; Shen, JW ; Yang, HJ ; Zhang, LJ ; Li, M ; Wang, JP
通讯作者: jwshen@scsio.ac.cn
关键词: Sedimentary facies ; Paleoenvironments ; Kalatar Formation ; Eocene ; Southwest Tarim Basin
刊名: FACIES
发表日期: 2014
卷: 60, 期:1, 页:111-131
收录类别: sci
部门归属: [Yang, Hong-Qiang ; Shen, Jian-Wei] Chinese Acad Sci, Key Lab Marginal Sea Geol, South China Sea Inst Oceanol, Guangzhou 510301, Guangdong, Peoples R China ; [Yang, Hong-Qiang] Univ Chinese Acad Sci, Beijing 100049, Peoples R China ; [Yang, Hai-Jun ; Zhang, Li-Juan ; Li, Meng] PetroChina Co Ltd, Tarim Oilfield Co, Korla 841000, Peoples R China ; [Wang, Jian-Po] Wuhan Ctr Geol Survey, Wuhan 430205, Peoples R China
项目归属: 海洋地质
资助者: National Natural Sciences Foundation of China [41240018, 40976030, 40976032]; Knowledge Innovation Program of South China Sea Institute of Oceanology [LYQY200806]
摘要: During the Eocene, the southwest Tarim Basin was a large epicontinental sea as a part of the Turun Sea in the eastern Paratethys. The marine succession of the Kalatar Formation is exposed along the piedmonts of the southern Tian Shan and western Kunlun Shan, and can be subdivided into three members. On the southern side of the Tarim Basin, a non-barrier shore-to-shelf, siliciclastic-dominated system, locally with carbonates and oyster biostromes, developed along the western Kunlun Shan, where river input led to a seaward arrangement of alluvial fan, foreshore, shoreface, and offshore facies. In contrast, on the northern side of the Tarim Basin, a carbonate ramp system formed along the southern Tian Shan, including shallow bioclastic-oolitic grainstone shoals, oyster beds, and red algal rudstones along with a number of evaporite units, which formed under hypersaline tidal-flat and lagoonal conditions. The basin center was a largely moderate deep and low-energy embayment facies. Deposition of the mixed carbonate-siliciclastic Kalatar Formation was controlled by tectonic activity, in particular the development of the Himalayan orogeny with the closure of Paratethys sea-level fluctuations, and arid-humid climate variations.
原文出处: 查看原文
WOS记录号: WOS:000329625100008
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内容类型: 期刊论文
URI标识: http://ir.scsio.ac.cn/handle/344004/10659
Appears in Collections:中科院边缘海地质重点实验室_期刊论文

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Recommended Citation:
Yang, HQ; Shen, JW; Yang, HJ; Zhang, LJ; Li, M; Wang, JP.Mixed carbonate-clastic facies in the Eocene Kalatar Formation of the southwest Tarim Basin (NW China): tectonic and climatic controls,FACIES,2014,60(1):111-131
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