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Distribution and origin of underground water chemical fields in Songliao continental oil-bearing sedimentary basin

机译:松辽大陆含油沉积盆地地下水化学场的分布与成因

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摘要

There are many factors affecting underground water chemistry of an oil-bearing sedi- mentary basin. The properties of underground water show variations in the vertical direction, giving rise to a vertical zonation with respect to underground water chemistry. Five zones could be divided downwards, including 1)the freshening zone due to meteoric water leaching(A); (2)the evaporation-concentration zone near the surface(B); 3)the freshening zone due to stra- tum compaction-released water(C_1)-infiltration-concentration zone during the mudstone com- paction and water releasing(C_2); 4)the freshening zone for clay mineral dehydration(D); and 5)the seepage-concentration zone (E).
机译:影响含油沉积盆地地下水化学的因素很多。地下水的特性在垂直方向上显示出变化,从而在地下水化学方面产生了垂直分区。可以分为五个区域,其中包括:1)由于水的淋滤而导致的新鲜区域(A); (2)在地表(B)附近的蒸发浓缩区; 3)泥岩压实时地层压实释放水(C_1)-渗透富集区(C_2)引起的清新区; 4)粘土矿物脱水的保鲜区(D); 5)渗流集中区(E)。

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