THE FORMATION, EVOLUTION OF MESO-CENOZOIC BASINS AND THEIR RELATIONSHIP TO OIL/GAS IN LINQING REGION
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摘要: 临清地区自三叠纪末—侏罗纪经历了拉张—挤压—拉张的交替更迭的地洼发展阶段。由于受边界条件的影响,控制两个地洼盆地发展期构造活动是多因素的,在盆地内形成的构造期也因地而异,故其内部构造显得十分复杂。Abstract: Linqing Region was experienced transformation from platform to Diwa(geodepression)stages during the period from Late Triassic to Early Jurassic.Severe extensions and faultdown took place during Jurassic-Early Cretace-ous and Paleogene,respectively.Thereafter,the two cycles of Mesozoic and Cenozoic Diwa(geodepression)basins and oil formations were formed.In addition to various basin types and complex structural patterns,combined with possible Paleozoic-Triassic platform type oil/gas in this region,it becomes a promising oil/gas prospect area.
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[1] 王尚文等,1983年:中国石油地质学,248页.石油工业出版社. [2] 叶连俊等,1983年:华北地台沉积建造.科学出版社. [3] 陈国达、费宝生,1980年:中国的地洼型油气田.石油与天然气地质.第1卷第3期.
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