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柴达木盆地南翼山地区新近系湖相碳酸盐岩成岩环境初探——碳、氧同位素和流体包裹体证据
引用本文:潘立银,黄革萍,寿建峰,刘占国.柴达木盆地南翼山地区新近系湖相碳酸盐岩成岩环境初探——碳、氧同位素和流体包裹体证据[J].矿物岩石地球化学通报,2009,28(1).
作者姓名:潘立银  黄革萍  寿建峰  刘占国
作者单位:中国石油杭州地质研究院,杭州,310023
摘    要:柴达木盆地南翼山地区新近系储层类型主要为湖相碳酸盐岩.用碳、氧同位素和流体包裹体方法研究湖相碳酸盐岩的形成环境结果表明,碳酸盐岩总体形成于高盐度环境,局部地区浅层样品在成岩过程中遭受过大气淡水的改造.根据孔隙充填胶结物中流体包裹体的均一温度,推断胶结物形成于储层深埋阶段,随后地层发生抬升,导致现今较低深度的包裹体样品具有较高的均一温度.

关 键 词:柴达木盆地  碳酸盐岩  碳氧同位素  流体包裹体

A Preliminary Study of Formation Environment of the Neogene Lacustrine Carbonates in Nanyishan Area of Qaidam Basin: Constrains from Carbon-Oxygen Isotope and Fluid Inclusion Analysis
PAN Li-yin,HUANG Ge-ping,SHOU Jian-feng,LIU Zhan-guo.A Preliminary Study of Formation Environment of the Neogene Lacustrine Carbonates in Nanyishan Area of Qaidam Basin: Constrains from Carbon-Oxygen Isotope and Fluid Inclusion Analysis[J].Bulletin of Mineralogy Petrology and Geochemistry,2009,28(1).
Authors:PAN Li-yin  HUANG Ge-ping  SHOU Jian-feng  LIU Zhan-guo
Institution:PAN Li-yin,HUANG Ge-ping,SHOU Jian-feng,LIU Zhan-guoHangzhou Institute of Petroleum Geology,CNPC,Hangzhou 310023,China
Abstract:The Neogene reservoir rocks in Nanyishan area of Qaidam basin are mainly lacustrine carbonates.Carbon-oxygen isotope compositions and fluid inclusion analyses were conducted in order to trace back the formation environment of the carbonates.Results indicated that the carbonates were precipitated in a high-salinity condition,and parts of the shallow carbonates were modified by meteoric water during diagenesis.Pore-filling cements were formed during the deep burial stage,and thereafter were uplifted as the st...
Keywords:Qaidam basin  carbonate rock  carbon-oxygen isotope  fluid inclusion  
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