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Reservoirs Distribution and Hydrocarbon Accumulation of Ordovician Carbonate in Tazhong Uplift, Tarim Basin

机译:塔里木盆地塔中隆起奥陶系碳酸盐岩储层分布与油气成藏

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Many types of marine carbonate reservoirs are discorvered in Tazhong Uplift, and the later alteration is obvious. The marine sources rock including the Cambrian-lower Ordovician and the midupper Ordovician provided a great deal of hydrocarbon for the hudrcarbon accumulation. The hydrocarbon filled into all kinds of reservoirs many times to form the different types of reservoirs in later Caledonian to early Hercynian epoch, later Hercynian to early Indo-Chinese epoch, later Yanshanian to Himalayan epoch. All these made the characteristics of hydrocarbon accumulation complex very much.
机译:在塔宏隆起中,许多类型的海洋碳酸盐储层在塔泽隆起中是令人着迷的,后来的改变是显而易见的。海洋来源岩石包括寒武纪下奥陶涅师和中间人奥陶诺维安为哈德柯布积累提供了大量的碳氢化合物。碳氢化合物很多时候填充了各种水库,以形成不同类型的水库,在后来的喀里多尼亚到早期的赫希尼亚时代,后来伊世纪到早期的印度 - 中国时代,后来燕山对喜马拉雅纪元。所有这些都是非常多的碳氢化合物积累复合物的特征。

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