松辽盆地梨树凹陷深部断陷沉积体系及层序地层特征 |
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引用本文: | 解习农.松辽盆地梨树凹陷深部断陷沉积体系及层序地层特征[J].石油实验地质,1994,16(2):144-151. |
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作者姓名: | 解习农 |
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作者单位: | 中国地质大学, 武汉 430074 |
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摘 要: | 松辽盆地梨树凹陷下部为断陷构造层序,上部为拗陷构造层序。断陷构造层序由四个层序组成,包括沙河子组下、中部,营城组和登娄库组。在深部断陷中广泛发育了冲积扇-扇三角洲体系、三角洲体系和湖泊体系沉积,其中湖泊体系沉积所占比例较大,构成梨树凹陷主要的烃源岩,辫状平原型扇三角洲砂体和三角洲砂体构成深部断陷主要储集层。本文在沉积体系和成因地层格架研究基础上,阐述深部断陷的层序地层及含油气性特征。
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关 键 词: | 松辽盆地 沉积体系 层序地层 |
收稿时间: | 1991-10-12 |
THE CHARACTERS OF THE DEPOSITIONAL SYSTEMS AND SEQUENCE STRATIGRAPHY OF THE DEEP FAULTDOWN DEPRESSION IN THE LISHU DEPRESSION OF THE SONGLIAO BASIN |
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Affiliation: | China Geological University |
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Abstract: | The Lishu Depression of the Songliao Basin can be divided into a faultdown depressionstructural sequence in the lower part and a depression structural sequence in the upperpart.The faultdown depression structural sequence could consist of four sub-sequences ofthe lower and middle parts of the Shahezi Formation,the Yingcheng Formation and theDeng louku Formation.In lower part of deep faultdown depression,the alluvial fan-fandelta system,delta system and lacustrine system are widespreaded,of which lacustrinesedimentary system takes a large proportion and could be considered as the main sourcerocks of hydrocarbons in the Lishu Depression,while the plaiting plains-type fan delta sandmassif and delta sand massif could be the main reservoirs in deep faultdown depression.This paper describes the stratigraphic sequence and petroliferous characters of deep fault-down depression based on the geological studies of the depositional systems and the forma-tion of sedimentary sequences. |
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