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  4. 中国科学院新生代地质与环境重点实验室
Facies analysis and depositional evolution of Lower-Middle Ordovician carbonates in the Shuntuoguole Low Uplift of Tarim Basin (NW China)

文献类型：期刊论文

作者Han, Jun3; Chen, Daizhao2; Cao, Zicheng3; Xiao, Chongyang3; Huang, Cheng3; Wang, Shi5; Chen, Jingping3; Guo, Chuan1,4
刊名FACIES
出版日期2024-02-01
卷号70期号:1页码:17
ISSN号0172-9179
关键词Carbonate ramp Depositional facies Sequence correlation Eustatic sea-level oscillations Early-Middle Ordovician
DOI10.1007/s10347-023-00676-5
英文摘要As a result of a deep burial depth (> 6.5 km), the depositional history of the Early to Middle Ordovician carbonate platform in the Shuntuoguole Low Uplift (Tarim Basin, NW China) has been difficult to unravel, leading to problems in understanding the controls of the facies distribution, particularly in terms of petroleum exploration. Integrated with geophysical surveys, detailed sedimentological observations document the platform evolution and show that a carbonate ramp system developed in the Shuntuoguole Low Uplift during the Early-Middle Ordovician, with twelve lithofacies types arranged into two facies associations, including peritidal to semi-restricted subtidal and open-marine subtidal facies. Based on the tempo-spatial distribution of lithofacies, seven third-order depositional sequences are identified, each composed of a transgressive lower package and a regressive upper part. Their sequence boundaries are commonly characterised by a transitional zone with no obvious subaerial exposure features. The correlation of relative sea-level (or accommodation space) changes derived from the vertical stacking pattern of facies with the global sea-level curve of Haq and Schutter (2008) and sea-level oscillations of coeval successions worldwide suggests that eustatic sea-level fluctuations were the overriding factor controlling the development and evolution of this carbonate ramp during the Early-Middle Ordovician. Meanwhile, regional or local tectonic subsidence and environmental factors (e.g. palaeoclimate and prevailing wind) also exerted an influence on the depositional processes of the Shuntuoguole Low Uplift over this time interval.
WOS关键词SEQUENCE STRATIGRAPHY ; CYCLIC CARBONATES ; FLUID INCLUSION ; NORTHWEST CHINA ; ISOTOPE ; AREA ; RAMP ; DOLOMITIZATION ; CONSTRAINTS ; RESERVOIRS
资助项目Guizhou Provincial Science and Technology Projects ; Northwest Oilfield Company ; SINOPEC ; Newly Established Project by the Ministry of Science and Technology of Sinopec[P23078] ; Cultivation Project of Guizhou University[[2019]68] ; Autonomous Region Tianshan Talent Program-Excellent Engineer Project ; [ZK[2021]]
WOS研究方向Geology ; Paleontology
语种英语
出版者SPRINGER
WOS记录号WOS:001120709200001
资助机构Guizhou Provincial Science and Technology Projects ; Guizhou Provincial Science and Technology Projects ; Northwest Oilfield Company ; Northwest Oilfield Company ; SINOPEC ; SINOPEC ; Newly Established Project by the Ministry of Science and Technology of Sinopec ; Newly Established Project by the Ministry of Science and Technology of Sinopec ; Cultivation Project of Guizhou University ; Cultivation Project of Guizhou University ; Autonomous Region Tianshan Talent Program-Excellent Engineer Project ; Autonomous Region Tianshan Talent Program-Excellent Engineer Project ; Guizhou Provincial Science and Technology Projects ; Guizhou Provincial Science and Technology Projects ; Northwest Oilfield Company ; Northwest Oilfield Company ; SINOPEC ; SINOPEC ; Newly Established Project by the Ministry of Science and Technology of Sinopec ; Newly Established Project by the Ministry of Science and Technology of Sinopec ; Cultivation Project of Guizhou University ; Cultivation Project of Guizhou University ; Autonomous Region Tianshan Talent Program-Excellent Engineer Project ; Autonomous Region Tianshan Talent Program-Excellent Engineer Project ; Guizhou Provincial Science and Technology Projects ; Guizhou Provincial Science and Technology Projects ; Northwest Oilfield Company ; Northwest Oilfield Company ; SINOPEC ; SINOPEC ; Newly Established Project by the Ministry of Science and Technology of Sinopec ; Newly Established Project by the Ministry of Science and Technology of Sinopec ; Cultivation Project of Guizhou University ; Cultivation Project of Guizhou University ; Autonomous Region Tianshan Talent Program-Excellent Engineer Project ; Autonomous Region Tianshan Talent Program-Excellent Engineer Project ; Guizhou Provincial Science and Technology Projects ; Guizhou Provincial Science and Technology Projects ; Northwest Oilfield Company ; Northwest Oilfield Company ; SINOPEC ; SINOPEC ; Newly Established Project by the Ministry of Science and Technology of Sinopec ; Newly Established Project by the Ministry of Science and Technology of Sinopec ; Cultivation Project of Guizhou University ; Cultivation Project of Guizhou University ; Autonomous Region Tianshan Talent Program-Excellent Engineer Project ; Autonomous Region Tianshan Talent Program-Excellent Engineer Project
源URL[http://ir.iggcas.ac.cn/handle/132A11/111523]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Guo, Chuan
作者单位1.Guizhou Univ, Coll Resources & Environm Engn, Key Lab Karst Georesources & Environm, Minist Educ, Guiyang 550025, Peoples R China
2.Chinese Acad Sci, Key Lab Cenozo Geol & Environm, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.Sinopec, Northwest Oilfield Co, Urumqi 830011, Peoples R China
4.Guizhou Univ, Minist Educ, Guizhou Karst Environm Ecosyst Observat & Res Stn, Guiyang 550025, Peoples R China
5.SINOPEC, Petr Explorat & Prod Res Inst, Beijing 100083, Peoples R China
推荐引用方式
GB/T 7714		 Han, Jun,Chen, Daizhao,Cao, Zicheng,et al. Facies analysis and depositional evolution of Lower-Middle Ordovician carbonates in the Shuntuoguole Low Uplift of Tarim Basin (NW China)[J]. FACIES,2024,70(1):17.
APA Han, Jun.,Chen, Daizhao.,Cao, Zicheng.,Xiao, Chongyang.,Huang, Cheng.,...&Guo, Chuan.(2024).Facies analysis and depositional evolution of Lower-Middle Ordovician carbonates in the Shuntuoguole Low Uplift of Tarim Basin (NW China).FACIES,70(1),17.
MLA Han, Jun,et al."Facies analysis and depositional evolution of Lower-Middle Ordovician carbonates in the Shuntuoguole Low Uplift of Tarim Basin (NW China)".FACIES 70.1(2024):17.

入库方式： OAI收割

来源：地质与地球物理研究所

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