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Multidisciplinary investigations exploring indicators of gas hydrate occurrence in the Krishna-Godavari Basin offshore, east coast of India

机译:探索印度东海岸克里希纳-哥达瓦里盆地天然气水合物发生指标的多学科研究

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We report some main results of multidisciplinary investigations carried out within the framework of the Indian National Gas Hydrate Program in 2002-2003 in the Krishna-Godavari Basin offshore sector, east coast of India, to explore indicators of likely gas hydrate occurrence suggested by preliminary multi-channel seismic reflection data and estimates of gas hydrate stability zone thickness. Swath bathymetry data reveal new evidence of three distinct geomorphic units representing (1) a delta front incised by several narrow valleys and mass flows, (2) a deep fan in the east and (3) a WNW-ESE-trending sedimentary ridge in the south. Deep-tow digital side-scan sonar, multi-frequency chirp sonar, and sub-bottom profiler records indicate several surface and subsurface gas-escape features with a highly resolved stratification within the upper 50 m sedimentary strata. Multi-channel seismic reflection data show the presence of bottom simulating reflections of continuous to discrete character. Textural analyses of 76 gravity cores indicate that the sediments are mostly silty clay. Geochemical analyses reveal decreasing downcore pore water sulphate (SO4 (2-)) concentrations (28.7 to < 4 mM), increasing downcore methane (CH4) concentrations (0-20 nM) and relatively high total organic carbon contents (1-2.5%), and microbial analyses a high abundance of microbes in top core sediments and a low abundance of sulphate-reducing bacteria in bottom core sediments. Methane-derived authigenic carbonates were identified in some cores. Combined with evidence of gas-escape features in association with bottom simulating reflections, the findings strongly suggest that the physicochemical conditions prevailing in the study area are highly conducive to methane generation and gas hydrate occurrence. Deep drilling from aboard the JOIDES Resolution during 2006 has indeed confirmed the presence of gas hydrate in the Krishna-Godavari Basin offshore.
机译:我们报告了2002-2003年在印度国家天然气水合物计划框架内在印度东海岸的克里希纳-戈达瓦里盆地近海部门进行的多学科研究的一些主要结果,以探讨初步的多水合物建议可能产生天然气水合物的指标通道地震反射数据和天然气水合物稳定带厚度估算。测深图数据揭示了三个不同的地貌单元的新证据,它们代表(1)由几个狭窄的山谷和质量流切割而成的三角洲前缘,(2)东部的一个深扇,以及(3)该地区的WNW-ESE趋势沉积脊南。深层数字侧扫声纳,多频chi声纳和下层剖面仪记录表明,地表和地下的气体逸出特征在上层50 m沉积岩层中具有高度分辨的分层。多通道地震反射数据表明存在连续到离散特征的底部模拟反射。对76个重力岩心的质地分析表明,沉积物主要是粉质粘土。地球化学分析显示,下层孔隙水硫酸盐(SO4(2-))浓度降低(28.7至<4 mM),下层甲烷(CH4)浓度增加(0-20 nM)和相对较高的总有机碳含量(1-2.5%)和微生物分析表明,顶芯沉积物中微生物含量高,而底芯沉积物中还原硫酸盐细菌的含量低。在某些岩心中发现了甲烷衍生的自生碳酸盐。结合与底部模拟反射相关的瓦斯逸出特征的证据,这些发现强烈表明,研究区域内普遍存在的物理化学条件非常有利于甲烷的产生和天然气水合物的产生。实际上,2006年在JOIDES决议上进行的深井钻探确实证实了克里希纳-戈达瓦里盆地近海存在天然气水合物。

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