这可以由沉积在不平坦的表面所引起，如邻近和覆于礁体构造之上，或靠近一生长断层，或缘于对压实作用不同的敏感性。
This can result from location on an uneven surface, such as near and over a reef structure, or near a growth fault, or from different susceptibility to compaction.
这可以由沉积在不平坦的表面所引起，如邻近和覆于礁体构造之上，或靠近一生长断层，或缘于对压实作用不同的敏感性。
This can result from location on an uneven surface, such as near and over a reef structure, or near a growth fault, or from different susceptibility to compaction.
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