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2D Basin-Scale Modeling of Accumulation of Gas Hydrates in Northern Slope of South China Sea

机译:南海北坡天然气水合物成藏的二维盆地尺度模拟

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A 2D software for modeling the accumulation of methane hydrates in basin scale was developed. This software couples models for the processes of methane generation from organic maters, the methane-bearing water migration from sediment consolidation, and kinetics of hydrate precipitation and accumulation. Based on the seismic interpretation, the geological information and geochemistry data, the dynamic accumulation of gas hydrates in northern slope of South China Sea was simulated. Dynamic accumulation and distribution of gas hydrates were found controlled by the tectonic evolution and the sediment fillings. The modeled fluid regime indicates that transverse migration become prefer ential that fluid migrates faster along the unconformable surfaces and faults with high permeability, towards the north edge of slpoe with a water depth of 1 200-1 500 m, where the hydrates may concentrated, the layer of 100 to 300 mbsf hi hydrate stability zone to found favorable for gas hydrates accu mulation.
机译:开发了用于模拟盆地规模中甲烷水合物积累的二维软件。该软件将有机物生成甲烷的过程,沉积物固结中含甲烷的水迁移以及水合物沉淀和累积动力学的模型耦合在一起。基于地震解释,地质信息和地球化学数据,模拟了南海北坡天然气水合物的动态聚集。发现天然气水合物的动态积累和分布受构造演化和沉积物充填的控制。模拟的流体状态表明,横向迁移成为优选的,流体沿着不整合面和高渗透率的断层更快地向水深为1 200-1 500 m的slpoe的北边缘迁移,水合物可能在那里浓缩,在100到300 mbsf的高水合物稳定区层中发现有利于天然气水合物的积聚。

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