贵州平塘甘寨剖面二叠系茅口组沉积特征与层序地层  

Sedimentary characteristics and sequence stratigraphy of the Permian Maokou Formation in the Ganzhai section,Pingtang,Guizhou

作　　者：李刚[1] 侯明才[1,2] 林良彪[1,2] 王文楷[1] 

机构地区：[1]成都理工大学油气藏地质及开发工程国家重点实验室,四川成都610059 [2]成都理工大学沉积地质研究院,四川成都610059

出　　处：《沉积与特提斯地质》2011年第1期19-27,共9页Sedimentary Geology and Tethyan Geology

基　　金：国家科技重大专项专题"南方海相碳酸盐岩层系大中型油气田规律与勘探评价"2008X05005-003-010HZ资助

摘　　要：本文应用沉积学手段对贵州平塘甘寨剖面中二叠统茅口组进行详细的沉积特征和层序地层的研究。研究结果显示,茅口组主要的岩石类型有亮晶-微晶生屑灰岩、生物灰岩、微晶灰岩、亮晶内碎屑灰岩、硅质岩、瘤状灰岩和含燧石灰岩等,茅口组生物种类有介形虫、腹足、腕足、三叶虫、藻类、棘屑、蜒、珊瑚、海百合茎等。岩石学特征和生物组合指示,平塘甘寨地区中二叠统茅口组为开阔碳酸盐台地沉积环境,包括台内滩和滩间两个亚相。茅口组可划分出3个Ⅲ级层序PSQ1、PSQ2和PSQ3,均由海侵体系域(TST)与高水位体系域(HST)两部分组成。层序发育受到了海平面升降变化控制,层序之间的界面P2q/PSQ1、PSQ1/PSQ2、PSQ2/PSQ3皆为岩性-岩相转换面,层序界面P3l/PSQ3在茅口末期受到东吴运动的影响,为构造不整合面。According to the sedimentological methods,the present paper deals,in detail,with the sedimentary characteristics and sequence stratigraphy of the Permian Maokou Formation in the Ganzhai section,Pingtang,Guizhou.The rock types of the Maokou Formation mainly consist of sparry-micritic bioclastic limestone,biogenic limestone,micritic limestone,intrasparite,siliceous rocks,nodular limestone and cherty limestone.The fossil types in the Formation comprise ostracods,gastropods,brachiopods,trilobites,algae,echinoderms,fusulinids,corals and crinoids.The lithology and fossils cited above indicate the open carbonate platform sedimentary environment of the Permian Maokou Formation.Three third-order sequences have been distinguished,including PSQ1,PSQ2 and PSQ3,all of which are built up of the transgressive（TST） and highstand（HST） systems tracts.The development of these sequences may be controlled by the sea-level changes.The sequence boundaries P2q/PSQ1,PSQ1/PSQ2 and PSQ2/PSQ3 represent lithologic-lithofacies transform surfaces.The sequence boundary P3l/PSQ3 exhibits a tectonic unconformity due to the influence of the Dongwu movement during the latest Maokouan.

关 键 词：贵州平塘 黔南坳陷 茅口组 沉积特征 层序地层 

分 类 号：TE121.34[石油与天然气工程—油气勘探]