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试论泌阳断陷双河-赵凹地区下第三系核三上段陆相层序中岩石地球化学旋回性特征
引用本文:胡受权,颜其彬.试论泌阳断陷双河-赵凹地区下第三系核三上段陆相层序中岩石地球化学旋回性特征[J].地球化学,1999(1).
作者姓名:胡受权  颜其彬
作者单位:西南石油学院
基金项目:“油气藏地质及开发工程”国家重点实验室开放基金
摘    要:泌阳断陷双河赵凹地区下第三系核三上段包括三个陆相层序,它们在岩石类型、矿物成分、化学成分及C、O同位素特征等方面,均呈现旋回性变化规律。据此,亦可作为划分和识别陆相层序的依据之一。

关 键 词:陆相层序  旋回性  岩石地球化学  下第三系  河南省

Lithologic geochemical cyclicity in terrigenous sequence of the upper member of Eh3 in Shuanghe Zhaoao, Biyang fault depression
Hu Shouquan,Yan Qibin.Lithologic geochemical cyclicity in terrigenous sequence of the upper member of Eh3 in Shuanghe Zhaoao, Biyang fault depression[J].Geochimica,1999(1).
Authors:Hu Shouquan  Yan Qibin
Abstract:The upper member of Eh3 consists of three terrigenous sequences for Shuanghe Zh aoao area, Biyang fault depression, and the sequences show cyclical changes and differential characteristics in lithological features, mineral compositions, che mical constituents and C and O isotopes. The lithologic geochemical cyclicity l aw can be used as one of evidences to divide and identify terrigenous sequences.
Keywords:terrigenous sequence  cyclicity  lithologic  geochemitry  Eogene  Hen an Province  
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