EARLY TERTIARY SEDIMENTARY ENVIRONMENT AND THE OIL AND GAS OF DONG MING DEPRESSION
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摘要: 东明凹陷是华北拗陷区南端的一个新生代沉积盆地,呈北北东向,北窄南宽,面积5000平方公里。凹陷为一早第三纪发育的地堑型断陷盆地。东侧以聊兰断层为界,西侧以长垣断层为界,北与临清地区的等县凹陷毗连,南隔胙城—兰考凸起与中牟凹陷时有相通。具有东部次凹带、西部次凹带、中央隆起带的"两凹一隆"构造格局。中原油田即位于凹陷的北部。Abstract: Dong Ming Depression is an early Tertiary block-faulting basin of graben type.The basin in-fillings are predominatingly clastic with subordinate lacustrine chemical rocks.Fluvial sediment developed only in Dong Ying Formation,The lacustrine sediments of Dong Ming Depression are devided into three sedimentary systems:lacustrine allochthonous clastic;and reworked sediments.It is thought that the alluvial fan subfacies,overbank and lake sub-facies,and gravitational current sediment sub-fades with different sedimentary backgrounds are characteristics of the sedimentary environment for block-faulting lake.The alluvial fan sand body and the gravitational current sand body are the major reservior for oil and gas;and the combined structural and lithological trap is the main type of oil and gas traps in Dong Ming Depression.
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[1] H.博歇特等,盐类矿床(中译本),地质出版社,1975年.
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