Sedimentology and Sequence Stratigraphy of Marine to Lacustrine Deltaic Deposits in a Craton Basin and Their Controlling Factors: Shan 2 Member-He 8 Member (Guadalupian-Lopingian, Permian), Southeast Ordos Basin, North China
Shan, Xin1,2; Yu, Xinghe3; Clift, Peter4; Li, Yalong5; Jin, Lina3; Su, Dongxu3; Du, Yonghui6; Zhou, Jinsong6; Han, Xiaoqin6
刊名ACTA GEOLOGICA SINICA-ENGLISH EDITION
2018-02
卷号92期号:1页码:268-285
关键词sequence stratigraphy sedimentary sequence delta marine to lacustrine evolution Roadian-Wuchiapingian Ordos Basin
ISSN号1000-9515
DOI10.1111/1755-6724.13505
英文摘要The Shan 2 Member, Shan 1 Member and He 8 Member of the Mid-Late Permian Shanxi and lower Xiashihezi formations, in the southeastern Ordos Basin, together comprise approximate to 150 m of deltaic deposits. This sequence records an overall evolution from deep marine environment to shallow lake associated with braided river, braided river delta and meandering river delta. Core description, well log interpretation, and stable isotope analysis, including carbon, oxygen and strontium, were conducted to understand the sedimentary evolution of Shan 2 to He 8 Member. The Shanxi Formation, which consists of the Shan 2 and Shan 1 members, is characterized by a tidal-influenced meandering river delta environment and a higher C-13 value and Sr-87/Sr-86 ratio and a lower O-18 value. The He 8 Member, the basal part of the Xiashihezi Formation, is featured by a braided river to braided river delta system and a lower C-13 value, Sr-87/Sr-86 ratio, and a higher O-18 value. Four third-order depositional sequences separated by five sequence boundaries are determined. Coarsening upward sequences of the Shan 2 Member-He 8 Member indicate a general regression trend, which can be correlated to global sea-level fall occurring during the Roadian-Wuchiapingian, as also evidenced by previous published zircon U-Pb results. The coal-bearing sequence (Shanxi Formation) to non-coal-bearing sequence (He 8 Member), as well as a decrease of Sr-87/Sr-86, suggest a trend from humid to arid climates. A combined effect of sea-level drop and a small uplift at the end of Shanxi Formation are proposed.
资助项目China Postdoctoral Science Foundation[2016M602087]
WOS关键词CARBON ; OXYGEN ; COLORADO ; MODEL ; SANDSTONES ; TECTONICS ; PLATEAU ; MARGIN ; AREA ; USA
WOS研究方向Geology
语种英语
出版者WILEY
WOS记录号WOS:000426255200019
内容类型期刊论文
源URL[http://ir.fio.com.cn:8080/handle/2SI8HI0U/25810]  
专题自然资源部第一海洋研究所
通讯作者Shan, Xin; Yu, Xinghe
作者单位1.State Ocean Adm, Inst Oceanog 1, Key Lab Marine Sedimentol & Environm Geol, Qingdao 266061, Shandong, Peoples R China
2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Peoples R China
3.China Univ Geosci, Sch Energy Resources, Beijing 100083, Peoples R China
4.Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA
5.Tongji Univ, Sch Ocean & Earth Sci, Shanghai 200092, Peoples R China
6.Shaanxi Yanchang Petr Grp Co Ltd, Res Inst, Xian 710065, Shaanxi, Peoples R China
推荐引用方式
GB/T 7714
Shan, Xin,Yu, Xinghe,Clift, Peter,et al. Sedimentology and Sequence Stratigraphy of Marine to Lacustrine Deltaic Deposits in a Craton Basin and Their Controlling Factors: Shan 2 Member-He 8 Member (Guadalupian-Lopingian, Permian), Southeast Ordos Basin, North China[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2018,92(1):268-285.
APA Shan, Xin.,Yu, Xinghe.,Clift, Peter.,Li, Yalong.,Jin, Lina.,...&Han, Xiaoqin.(2018).Sedimentology and Sequence Stratigraphy of Marine to Lacustrine Deltaic Deposits in a Craton Basin and Their Controlling Factors: Shan 2 Member-He 8 Member (Guadalupian-Lopingian, Permian), Southeast Ordos Basin, North China.ACTA GEOLOGICA SINICA-ENGLISH EDITION,92(1),268-285.
MLA Shan, Xin,et al."Sedimentology and Sequence Stratigraphy of Marine to Lacustrine Deltaic Deposits in a Craton Basin and Their Controlling Factors: Shan 2 Member-He 8 Member (Guadalupian-Lopingian, Permian), Southeast Ordos Basin, North China".ACTA GEOLOGICA SINICA-ENGLISH EDITION 92.1(2018):268-285.
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