论文成果

Mesozoic and Cenozoic tectono-thermal reconstruction of the western Bohai Bay Basin (East China) with implications for hydrocarbon generation and migration

摘要:Studies on the tectono-thermal evolution of the western Bohai Bay Basin (WBBB), including the Jizhong Subbasin and Cangxian Uplift, are important for further petroleum exploration and exploitation. This study aims to reconstruct the tectono-thermal history of the WBBB based on a combination of 125 vitrinite reflectance (Ro) data and seven apatite fission track (AFT) and nine apatite (U-Th)/He (AHe) ages. The effective AFT ages range from 60.3 to 97.0 Ma, with mean track lengths of 10.86-12.64 mu m. The variable single-grain AFT ages are explained to be due to the parameter D-par. The effective Alie ages range from 21.1 Ma to 75.0 Ma. Two rapid cooling events revealed by the thermal modeling results occurred during the Early-Late Cretaceous (130-90 Ma) and Late Eocene-Early Miocene (40-18 Ma), respectively. The Fuping Complex, which is located in the western margin of the WBBB and mainly composed of the Paleo-proterozoic high-grade gneisses, experienced the intensive extension-detachment during the Early-Late Cretaceous along with the subduction of the Izanagi Plate, that was probably responsible for the first cooling event. The second cooling event was caused by the subduction of the Pacific Plate during the Middle Eocene-Early Miocene (43-23 Ma), as well as the collision of the Indian and Eurasian Plates and the rollback of the subducting Pacific Plate during the Early Miocene (23-18 Ma). The WBBB experienced two heat flow peaks of similar to 75 and similar to 80 mW/m(2) during the Early Cretaceous and the Late Eocene, respectively. During the Late Eocene-Early Miocene, rapid subsidence in the Baxian Depression (one secondary tectonic unit of the Jizhong Sub-basin) coupled with the rapid uplift in the Cangxian Uplift caused the Shahejie Formation of the middle-upper Eocene to generate gas during the Early Miocene. Meanwhile, tectonic movement during the Early Miocene also caused faults to become migration paths, as revealed by the homogenization temperature of the fluid inclusion. This study provides new insights regarding the tectonic and hydrocarbon evolution of the WBBB.

关键字:Western Bohai Bay Basin Apatite fission track Apatite (U-Th)/He Tectono-thermal evolution Hydrocarbon maturation Hydrocarbon migration

ISSN号:1367-9120

卷、期、页:卷: 160 页: 380-395

发表日期:2018-07-01

期刊分区(SCI为中科院分区):三区

收录情况:SCIE(科学引文索引网络版),ESI(基本科学指标数据库)

发表期刊名称:JOURNAL OF ASIAN EARTH SCIENCES

参与作者:赵贤正

通讯作者:沈芳宇,刘念,许威

第一作者:常健,邱楠生

论文类型:期刊论文

论文概要:常健,邱楠生,赵贤正,沈芳宇,刘念,许威,Mesozoic and Cenozoic tectono-thermal reconstruction of the western Bohai Bay Basin (East China) with implications for hydrocarbon generation and migration,JOURNAL OF ASIAN EARTH SCIENCES,2018,卷: 160 页: 380-395

论文题目:Mesozoic and Cenozoic tectono-thermal reconstruction of the western Bohai Bay Basin (East China) with implications for hydrocarbon generation and migration