Kendong 32 fault block is a typical heavy oil reservoir with loose sandstone.
垦东32断块属于典型的疏松砂岩稠油油藏。
Field study reveals that the near surface structure in Kendong, Shengli Oilfield consists of interbeds of low velocity mud formation and high velocity sands.
通过野外试验和调查，查明了垦东地区的表层是一种低速泥层与高速沙板层的互层结构。
Through the analysis on stress field, palaeogeomorphology and spatial distribution of faults, Kendong region is considered to be 'concealed' strike - slip fault.
通过对区域应力场、古地貌和断裂空间展布等分析，认为垦东地区发育“隐伏型”走滑断裂。
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