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TECTONIC EVOLUTION OF THE KONGDIAN FORMATION──SHA-Ⅳ MEMBER IN THE HUIMIN DEPRESSION AND THE DONGYING DEPRESSION
dai junsheng(department of mining; chinese university of mining; beijing 100083)absteact:the kongdian formation and the sha- member are important oil-gas bearing levels in the huimin depression and the dongying depression. the tectonic evolution there can be divided into four stages: the filling stage of extensional semi-grabens corresponding for the kongdian formation -- sha- member; the strong block-activity stage corresponding for the sha- and sha- members; the block-activity complicating stage corresponding for the sha- member-dongying formation; and the deep burying stage corresponding for neogene and quaternary. the evolution order of faults is tubular listric slope-flat. the evolution orders of these two depressions during eogene are rotational send-graben rolling semi-graben compound semi-graben. meanwhile the subsidence centers migtated from west to east. the extensional strength was the maximal in the time corresponding to the kongdian formation sha- member in the huimin depression but the maximal in time corresponding to the sha- and sha members in the dongying depression. tectonic traps were formed mostly in the time corresponding to the sha- and sha- members and secondly in the time corresponding to the sha- member-dongytng formation.
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ripples in overwater plains of the yellow river delta
zhong jianhua (department of petroleum resource science; university of petroleum; dongying; shandong province257062)wang jianbao (scientific and technical office; administrative bureau of petroleum; shengli oil field; dongying; shandong province. 257062)
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