Downward shift of gas hydrate stability zone due to seafloor erosion in the eastern Dongsha Island,South China Sea

被引：0
|
作者：
JIN Jiapeng [1 ,2 ,3 ]
WANG Xiujuan [1 ,2 ,3 ,4 ]
HE Min [5 ]
LI Jie [5 ]
YAN Chengzhi [5 ]
LI Yuanping [5 ]
ZHOU Jilin [1 ,3 ]
QIAN Jin [1 ,2 ,4 ]
机构：
[1] Key Laboratory of Marine Geology and Environment & Center of Deep-Sea Research, Institute of Oceanology, Chinese Academy of Sciences
[2] Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology (Qingdao)
[3] Center for Ocean Mega-Science, Chinese Academy of Sciences
[4] University of Chinese Academy of Sciences
[5] Shenzhen Branch of China National Offshore Oil Corporation Ltd
来源：
JournalofOceanologyandLimnology | 2020年 / 38卷 / 04期
基金：
国家重点研发计划; 国家高技术研究发展计划(863计划); 中国国家自然科学基金;
关键词：
bottom simulating reflections(BSRs); downward shift; seafloor erosion; gas hydrate dissociation;
D O I：
暂无
中图分类号：
P618.13 [石油、天然气]; P631.46 [];
学科分类号：
摘要：
New acquired and reprocessed three-dimensional(3 D) seismic data were used to delineate the distribution and characterization of bottom simulating reflections(B SRs) in the Chaoshan Sag,in the eastern part of Dongsha Island,South China Sea.Three submarine canyons with different scales were interpreted from the 3 D seismic data,displaying three stages of canyon development and are related with the variation of BSR.Abundant faults were identified from the coherence and ant-tracing attributions extracted from3 D seismic data,which provide the evidence for fluid migration from deeper sediments to the gas hydrate stability zone(GHSZ).The uplift of Dongsha Island created a large number of faults and leads to the increased seafloor erosion.The erosion caused the cooling of the seafloor sediments and deepening of the base of the gas hydrate stability zone,which is attributed to the presence of paleo-BSR and BSR downward shift in the study area.Hence,methane gas may be released during the BSR resetting and gas hydrate dissociation related with seafloor ero sion.
引用
收藏
页码：1188 / 1200
页数：13
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