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滦平盆地上白垩统九佛堂组中的熔积岩及地质意义
引用本文:张英利,孟庆任,渠洪杰.滦平盆地上白垩统九佛堂组中的熔积岩及地质意义[J].沉积学报,2008,26(1):105-110.
作者姓名:张英利  孟庆任  渠洪杰
作者单位:西安石油大学油气资源学院,西安,710065;中国科学院地质与地球物理研究所,北京,100029;中国地质科学院地质力学研究所,北京,100081
摘    要:通过对滦平盆地沉积地层的野外观察,系统分析了九佛堂组的沉积特征及其变化规律,鉴别出特殊的岩石类型——熔积岩;较详细的描述了熔积岩所在剖面的沉积特征,最后结合盆地的区域地质背景,初步认为滦平盆地为火山—沉积盆地,强烈的同沉积构造运动伴随岩浆活动,致使盆地九佛堂组沉积地层内发育熔积岩。

关 键 词:熔积岩  滦平盆地  早白垩世  九佛堂组
文章编号:1000-0550(2008)01-0105-06
收稿时间:2007-03-28
修稿时间:2007-05-05

Peperite in the Jiufotang Formation of the Luanping Basin and Its Geological Implications
ZHANG Ying-li,MENG Qing-ren,QU Hong-jie.Peperite in the Jiufotang Formation of the Luanping Basin and Its Geological Implications[J].Acta Sedimentologica Sinica,2008,26(1):105-110.
Authors:ZHANG Ying-li  MENG Qing-ren  QU Hong-jie
Institution:School of Petroleum Resources, Xi'an Shiyou University, Xi'an 710065
Abstract:Based on observation in the field,this paper documents the sedimentary features and variations of Jiufotang Formation in the Luanping basin.A special kind of rock,namely,peperite,was identified and described in detail.Taking the geological setting of the basin into account,the author believes that the Luanping basin is a volcanic sedimentary basin.The intensive synsedimentary tectonic activity has resulted in the peperite in the Jiufotang Formation.
Keywords:Peperite  Luanping Basin  Early Cretaceous  Jiufotang Formation
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