Search
E-mail
RSS

Online submission Editor-in-chief Peer review Staff Login

Journal of Tropical Oceanography >

2013 , Vol. 32 >Issue 4: 22 - 29

DOI: https://doi.org/10.11978/j.issn.1009-5470.2013.04.004

The survey status and geological conditions of accumulation of gas hydrate resource in the East China Sea

Expand
  • 1. Key Laboratory of Marine Hydrocarbon Resource and Environment Geology, Qingdao Institute of Marine Geology, Ministry of Land and Resources, Qingdao 266071, China; 2. China University of Petroleum, Qingdao 266580, China

Received date: 2011-09-06

  Revised date: 2012-03-27

  Online published: 2013-10-30

Fold

Abstract

This paper provides a comparative analysis of the geological conditions of the gas hydrate formation and evolution in the East China Sea. It shows occurrence evidence of cold seeps and carbon dioxide hydrate, which is based on the recall of gas hydrate survey status quo. There are many types of BSR(bottom simulating reflector) in the study area, such as the continental slope, the low uplift, deep-sea plains and so on, according to the explanation of BSR profile characteristics of conventional two-dimensional seismic and high-resolution seismic, and the explanation of signal processing and speed fine processing analysis. An estimation of natural gas hydrate resources by the measured seabed organic carbon, porosity and new edition of gas hydrate phase diagram is carried out.

Key words： East China Sea slope; geological background; gas hydrate; type features of BSR; geological conditions of accumulation

Cite this article

XU Hong, CAI Ying, SUN He-qing, YAN Gui-jing, WEI Kai, ZHAO Xin-wei, ZHU Yu-rui, SHI Jian, DONG Gang, LI Qing . The survey status and geological conditions of accumulation of gas hydrate resource in the East China Sea[J]. Journal of Tropical Oceanography, 2013 , 32(4) : 22 -29 . DOI: 10.11978/j.issn.1009-5470.2013.04.004

References

[1]杨文达, 陆文才.东海陆坡——冲绳海槽天然气水合物初探[J]. 海洋石油, 2000, 20(4): 23-28.
[2]方银霞, 黎明碧, 金翔龙. 东海冲绳海槽天然气水合物的资源前景[J]. 天然气地球科学, 2001. 12(6): 32-37.
[3]栾锡武, 秦蕴珊. 冲绳海槽宫古段西部槽底海底气泉的发现[J].科学通报, 2005, 50(8): 802-810.
[4]孟宪伟, 刘保华, 石学法, 等. 冲绳海槽中段西陆坡下缘天然气水合物存在的可能性分析[J]. 沉积学报, 2000, 18(4): 629-633.
[5]赵金海, 唐建, 王舜杰. 冲绳海槽新生代构造演化讨论[J].海洋石油, 2003, 23(3): 1-9.
[6]黄奇瑜. 台湾西南部天然气水合物的调查研究报告[R]. 青岛: 青岛海洋地质研究所. 2001.
[7]INAGAKI F, KUYPERS M M M, TSUNOGAI U, et al. Microbial community in a sediment-hosted CO2 lake of the southern Okinawa Trough hydrothermal system [J]. PNAS, 2006, 103 (38): 14164-14169.
[8]许红, 刘守全, 王建桥, 等. 天然气水合物物理化学状态平衡及其在冲绳海槽的应用[J]. 海洋地质动态, 2001, 17(7): 8-13.
[9]NEALSON K. Lakes of liquid CO2 in the deep sea [J]. PNAS, 2006, 103(38): 13903-13904.
[10]周琦, 陈建华, 张命桥, 等.冷泉碳酸盐岩研究进展及成矿意义[J].贵州科学, 2007, 25(增刊): 103-110.
[11]А.Ю.Леин.产自黑海和挪威海的冷甲烷渗透流[J]. 朱佛宏, 译. 海洋地质动态, 2006, 22 (9) : 25-26.
[12]MOORE J C, BROWN K M, HORATH F, et al. Plumbing accretionary prisms[M]//TARNEY J, PICKERING K T, KNIPE R J, et al. The Behavior and Influence of Fluids in Subduction Zones. London: The Royal Society, 1991: 49-62.
[13]MOORE J C, VROLIJK P. Fluids in accretionary prisms[J]. Reviews of Geophysics, 1992, 30: 113-135.
[14]陈忠, 杨华平, 黄奇瑜, 等. 海底甲烷冷泉特征与冷泉生态系统的群落结构[J].热带海洋学报, 2007, 26(6): 73-82.
[15]杨文达, 曾久岭, 王振宇. 东海陆坡天然气水合物成矿远景[J]. 海洋石油, 2004, 24(2): 1-8.
[16]方银霞, 高金耀, 黎明碧等. 冲绳海槽天然气水合物与地质构造的关系[J]. 海洋地质与第四纪地质, 2005, 25(1): 85-91.
[17]栾锡武, 高金耀, 梁瑞才, 等. 冲绳海槽宫古段中央地堑的形态与分布[J]. 地质学报, 2006, 80(8): 1149-1155.
[18]栾锡武, 鲁银涛, 赵克斌, 等. 东海陆坡及邻近槽底天然气水合物成藏条件分析及前景[J]. 现代地质, 2008, 22(3): 342-355.
[19]徐宁, 吴时国, 王秀娟, 等. 东海冲绳海槽陆坡天然气水合物的地震学研究[J]. 地球物理学进展, 2006, 21(2): 564-571.
[20]赵汗青, 时国, 徐宁, 等.东海与泥底辟构造有关的天然气水合物初探[J]. 现代地质, 2006, 20(1): 115-122.
Options
Outlines

/

〈 〉