樊茹,卢远征,张学磊,张师本,王志浩,李鑫,邓胜徽,张放

• 1:中国石油勘探开发研究院
• 2:提高采收率国家重点实验室
• 3:中国石油天然气集团公司油气储层重点实验室
• 4:中国科学院南京地质古生物研究所

摘要(Abstract)：

贵州习水良村剖面地层发育齐全,是目前所知上扬子地区出露最为完整的奥陶系剖面之一。该剖面海相碳酸盐岩发育,具备优越的牙形石生物地层研究条件。本次,笔者等于此获得了丰富的牙形石标本,经研究建立了16个牙形石带,由下至上分别为Monocostodus sevierensis带,Cordylodus angulatus带,Glyptoconus quadraplicatus带,Tripodus proteus带,Triangulatus bifidus带,Serratognathus diversus带,Oepikodus communis带,Oepikodus evae带,Baltoniodus triangularis带,Baltoniodus navis带,Paroistodus originalis带,Baltoniodus aff.navis带,Lenodus antivariabilis-L.variabilis组合带,Pygodus serra带,Hamarodus brevirameus带以及Protopanderodus insculptus带。

关键词(KeyWords)： 生物地层;牙形石;地层剖面;奥陶系;习水;贵州

Abstract:

Keywords:

基金项目(Foundation): 国家重大科技专项“大型油气田及煤层气开发”(编号2008ZX05004-001;2011ZX05004-002);; 中国石油天然气股份有限公司“十一五”重大科技专项“海相碳酸盐岩大油气田勘探开发关键技术”;; 中国石油天然气股份公司“十二五”重大科技项目“四新”项目06课题(2014A0216);; 中国科学院南京地质古生物所“奥陶-志留系资源地层学”博士后项目的资助与研究成果

作者(Author): 樊茹,卢远征,张学磊,张师本,王志浩,李鑫,邓胜徽,张放

DOI: 10.19839/j.cnki.dcxzz.2015.01.002

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