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箕状断陷盆地缓坡带层序格架特征与演化--以济阳坳陷为例
引用本文:彭传圣.箕状断陷盆地缓坡带层序格架特征与演化--以济阳坳陷为例[J].华东地质学院学报,2005,28(3):239-243.
作者姓名:彭传圣
作者单位:[1]中国科学院地质与地球物理研究所,北京 100029 [2]胜利油田有限公司地质科学研究院,山东 东营 257000
基金项目:国家“十五”科技攻关项目(2003BA613A)
摘    要:依据缓坡带对层序类型、地层结构特征的控制及地貌特征、成因将济阳坳陷缓坡带分为单断-沉积坡折型、单断-斜坡型和双断-构造坡折型三种类型.三种缓坡类型构造-沉积演化背景不同,形成了不同的层序格架特征.济阳断陷盆地的构造演化史决定了较完整的缓坡带层序演化由双断-构造坡折型向单断-沉积坡折型再向单断-斜坡型演化.

关 键 词:箕状断陷盆地  济阳坳陷  缓坡带  层序  格架  演化
文章编号:1000-2251(2005)03-239-05
收稿时间:2005-01-22
修稿时间:2005年1月22日

Sequence Framework Feature and Evolution of the Ramp Belt of Half-Graben-Basin--Example of Jiyang Depression
Peng ChuanSheng.Sequence Framework Feature and Evolution of the Ramp Belt of Half-Graben-Basin--Example of Jiyang Depression[J].Journal of East China Geological Institute,2005,28(3):239-243.
Authors:Peng ChuanSheng
Abstract:Based on ramp belt control the sequence type and the features of strata structure along with its physiognomy feature and the cause of formation, Jiyang depression ramp can be classified into three types of single fault-sedimentary, double fault-structural slope break type and single fault-clinoform type. As a result of the different structural-sedimentary evolvement background, there formed distinct features of sequence framework. The structural evolvement history of Jiyang depression results in comparatively whole sequence evolvement of gentle slope belt, that is transition from double fault-structural to single fault-sedimentary slope break type, and then to single fault-clinoform type.
Keywords:half-graben basin  Jiyang depression  ramp belt  sequence  framework  evolution
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