Gas hydrate accumulation associated with fluid escape structure in the western margin of South China Sea
作者机构:PetroChina Hangzhou Research Institute of GeologyHangzhou 310023China CAS Key Laboratory of Ocean and Marginal Sea GeologySouth China Sea Institute of OceanologyChinese Academy of SciencesGuangzhou 510301China
出 版 物:《Journal of Oceanology and Limnology》 (海洋湖沼学报(英文))
年 卷 期:2023年第41卷第3期
页 面:947-958页
核心收录:
学科分类:081803[工学-地质工程] 08[工学] 0818[工学-地质资源与地质工程] 0824[工学-船舶与海洋工程]
基 金:Supported by the China Academy of Petroleum Exploration and Development(Nos.2019B-4909,2021DJ2401) Dr.Wei LI is specially funded by the CAS Pioneer Hundred Talents Program(No.Y8SL011001)
主 题:gas hydrate fluid-escape structures gas sources bottom simulating reflector(BSR) South
摘 要:Gas hydrates have been found in the western continental margin of South China Sea,which are revealed by widespread bottom simulating reflectors(BSRs)imaged from a three-dimensional(3D)seismic volume near the Guangle carbonate platform in the western South China ***-escape structures(faults and gas chimneys)are originated below BSR were distinguished.A comprehensive model in three-level structure was proposed to depict the gas hydrate accumulation in the study *** Level 1,regional major faults and gas chimneys provide the first pathways of upward migration of gas near *** Level 2,pervasive polygonal faults in carbonate layer promote the migration of *** Level 3,gases sourced from near-basement accumulate within shallow sediment layers and form gas hydrate above the unit with faults once appropriate temperature and pressure *** gas hydrates in the study area are mainly in microbial origin,and their accumulation occurs only when fluid-escape structures align in all the three *** proposed model of the gas hydrate accumulation in western SCS margin provides new insights for further studies in this poorly studied area.