Estimation of methane flux offshore SW Taiwan and the influence of tectonics on gas hydrate accumulation

NCU Institutional Repository > 地球科學學院 > 地球物理研究所 > 期刊論文 > Item 987654321/50519

jsp.display-item.identifier=請使用永久網址來引用或連結此文件: http://ir.lib.ncu.edu.tw/handle/987654321/50519

题名:	Estimation of methane flux offshore SW Taiwan and the influence of tectonics on gas hydrate accumulation
作者:	Chuang,PC;Yang,TF;Hong,WL;Lin,S;Sun,CH;Lin,ATS;Chen,JC;Wang,Y;Chung,SH
贡献者:	地球物理研究所
关键词:	CONTINENTAL-MARGIN SEDIMENTS;TATUN-VOLCANO GROUP;SOUTHWESTERN TAIWAN;MARINE-SEDIMENTS;MUD VOLCANOS;ACCRETIONARY PRISM;SULFATE REDUCTION;CORED SEDIMENTS;NORTHERN TAIWAN;COLLISION ZONE
日期:	2010
上传时间:	2012-03-27 17:36:00 (UTC+8)
出版者:	國立中央大學
摘要:	Widely distributed bottom simulating reflectors (BSRs) imply the potential existence of gas hydrates offshore southwestern Taiwan. To compare the distribution of methane concentrations along passive and active margins in the region, bottom waters and cored sediments were collected during four cruises from 2005 to 2006. The results reveal that sites with high methane concentrations are predominantly distributed in the active margin and site GS5 is the only site that contains very high methane concentrations in the passive margin of studied area. Anomalously high methane fluxes still can be obtained from the calculation of diffusive methane flux, although there might be some gas leakage during or after sampling procedures. The profiles of methane and sulfate concentration reveal very shallow depths of the sulfate-methane interface (SMI) at some sites. There is evidence that sulfate reduction is mainly driven by the process of anaerobic methane oxidation. Thus, sulfate fluxes can be used as a proxy for methane fluxes through the use of diffusion equations; and the results show that the fluxes are very high in offshore southwestern Taiwan. The depths of the SMI are different at sites GH6 and C; however, both methane profiles reveal parallel methane gradients below the SMI. This might be because of methane migration to surface sediments from the same reservoir with the same diffusion rates. Although BSRs are widely distributed both in the active margin and in the passive margin, most sites with high methane concentrations have been found in the active margin. Therefore, the specific tectonic settings in offshore SW Taiwan might strongly control the stability of gas hydrates, and thus affect the methane concentrations and fluxes of the sediments and sea waters. Furthermore, the carbon isotopic composition of methane shows that a biogenic gas source is dominant at shallower depth; however, some thermogenic gases might be introduced through the fracture/fault zones from deeper source in the active region of studied area.
關聯:	GEOFLUIDS
显示于类别:	[地球物理研究所] 期刊論文

文件中的档案:

档案	描述	大小	格式	浏览次数
index.html		0Kb	HTML	528	检视/开启

在NCUIR中所有的数据项都受到原著作权保护.

社群 sharing

数据加载中.....