2012•Acta Scientiarum Naturalium Universitatis SunyatseniRequires access
Comparison of basic features and origins of oolitic shoal reservoirs between carbonate platform interior and platform margin locations in the Lower Triassic Feixianguan Formation of the Sichuan Basin,southwest China
Tan, Xiucheng, Zhao Zhao, Luzi, Luo, Jiang, Xingfu, Cao, Jian JIAN, Liu, Hong, Li, Ling, Wu, Xingbo, Nie, Yong
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Abstract
9% 孔并且 > 0.1 mD 渗透) 并且毛孔喉咙结构比内部水库。这些差别被两个主要 depositional 特征和第二等的成岩作用影响。为内部碳酸盐，水库，早大气的溶解，弱压缩和强壮的硬化是重要的控制因素。由对比，控制边缘碳酸盐水库的形成的因素主要包括化成白云石，主要毛孔的保藏和埋葬溶解。