Meso-Cenozoic Tectono-Thermal Evolution History in Bohai Bay Basin, North China

doi:10.1007/s12583-014-0500-0

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 中国科学院页岩气与地质工程重点实验室

	Meso-Cenozoic Tectono-Thermal Evolution History in Bohai Bay Basin, North China
	Zuo, Yinhui 1,2; Qiu, Nansheng 2; Li, Jiawei 3; Hao, Qingqing 4; Pang, Xiongqi 2; Zhao, Zhongying 5; Zhu, Qi 6
刊名	JOURNAL OF EARTH SCIENCE
	2015-06-01
卷号	26 期号:3 页码:352-360
关键词	Bohai Bay Basin Meso-Cenozoic thermal history vitrinite reflectance apatite fission track
DOI	10.1007/s12583-014-0500-0
文献子类	Article
英文摘要	The thermal history of sedimentary basins is a key factor for hydrocarbon accumulation and resource assessment, and is critical in the exploration of lithospheric tectono-thermal evolution. In this paper, the Cenozoic thermal histories of nearly 200 wells and the Mesozoic thermal histories of 15 wells are modeled based on the vitrinite reflectance and apatite fission track data in Bohai Bay Basin, North China. The results show that the basin experienced Early Cretaceous and Paleogene heat flow peaks, which reveals two strong rift tectonic movements that occurred in the Cretaceous and the Paleogene in the basin, respectively. The thermal evolution history in Bohai Bay Basin can be divided into five stages including (1) the low and stable heat flow stage from the Triassic to the Jurassic, with the heat flow of 53 to 58 mW/m(2); (2) the first heat flow peak from the Early Cretaceous to the middle of the Late Cretaceous, with a maximum heat flow of 81 to 87 mW/m(2); (3) the first post-rift thermal subsidence stage from the middle of the Late Cretaceous to the Paleocene, with the heat flow of 65 to 74 mW/m(2) at the end of the Cretaceous; (4) the second heat flow peak from the Eocene to the Oligocene, with a maximum heat flow of 81 to 88 mW/m(2); and (5) the second thermal subsidence stage from the Neogene to present, with an average heat flow of 64 mW/m(2).
WOS关键词	THERMAL HISTORY ; EAST CHINA ; GEOTHERMAL REGIME ; PETROLEUM-EXPLORATION ; JIYANG DEPRESSION ; APATITE ; AREA ; TEMPERATURE ; SUBSIDENCE ; KINETICS
WOS研究方向	Geology
语种	英语
WOS记录号	WOS:000355498500006
资助机构	National Natural Science Foundation of China(41402219 ; National Natural Science Foundation of China(41402219 ; Key State Science and Technology Project(2011ZX05006) ; Key State Science and Technology Project(2011ZX05006) ; 41125010 ; 41125010 ; 91114202) ; 91114202) ; National Natural Science Foundation of China(41402219 ; National Natural Science Foundation of China(41402219 ; Key State Science and Technology Project(2011ZX05006) ; Key State Science and Technology Project(2011ZX05006) ; 41125010 ; 41125010 ; 91114202) ; 91114202)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/62502]
专题	地质与地球物理研究所_中国科学院页岩气与地质工程重点实验室
作者单位	1.Chengdu Univ Technol, Coll Energy Resources, Chengdu 610059, Peoples R China 2.China Univ Petr, State Key Lab Petr Resource & Prospecting, Beijing 102249, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Engn Geomech, Beijing 100029, Peoples R China 4.China Met Geol Bur, Inst Mineral Resource Res, Beijing 100025, Peoples R China 5.PetroChina Res Inst Petr Explorat, Beijing 100083, Peoples R China 6.China Natl Offshore Oil Corp, Zhanjiang Oil Co, Zhanjiang 524057, Peoples R China
推荐引用方式 GB/T 7714	Zuo, Yinhui,Qiu, Nansheng,Li, Jiawei,et al. Meso-Cenozoic Tectono-Thermal Evolution History in Bohai Bay Basin, North China[J]. JOURNAL OF EARTH SCIENCE,2015,26(3):352-360.
APA	Zuo, Yinhui.,Qiu, Nansheng.,Li, Jiawei.,Hao, Qingqing.,Pang, Xiongqi.,...&Zhu, Qi.(2015).Meso-Cenozoic Tectono-Thermal Evolution History in Bohai Bay Basin, North China.JOURNAL OF EARTH SCIENCE,26(3),352-360.
MLA	Zuo, Yinhui,et al."Meso-Cenozoic Tectono-Thermal Evolution History in Bohai Bay Basin, North China".JOURNAL OF EARTH SCIENCE 26.3(2015):352-360.