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巴楚地区碳酸盐岩中深成侵入岩特征及其对储层发育的影响
引用本文:聂保锋,于炳松,朱金富.巴楚地区碳酸盐岩中深成侵入岩特征及其对储层发育的影响[J].地学前缘,2008,15(2):90-99.
作者姓名:聂保锋  于炳松  朱金富
作者单位:中国地质大学,地质过程与矿产资源国家重点实验室,北京,100083
基金项目:国家重点基础研究发展计划(973计划)
摘    要:为了深入探讨深部岩浆活动对碳酸盐岩储层发育的影响,文中通过显微鉴定、地球化学分析以及流体包裹体测试,对巴楚地区和3井奥陶纪钻遇的火成岩进行了详细研究。和3井碳酸盐岩中的火成岩是紫苏辉长岩,为深成侵入岩体,辉长岩的w(SiO2)介于44.89%~45.39%,w(K2O+Na2O)为4.04%~4.67%,w(Na2O)/w(K2O)为2.16~4.23,属钠质碱性系列,形成于板内构造环境。微量元素分配模式以Ba富集Sr亏损为特征。∑REE介于163.43×10-6~215.99×10-6,LREE/HREE介于5.14~5.58,LaN/YbN介于5.192~5.980,δEu介于0.926~1.002,稀土配分模式属轻稀土富集型,通过对和3井碳酸盐岩孔隙度、渗透率以及其中流体包裹体的分析,孔隙度和渗透率的变化与辉长岩的分布有关,流体包裹体温度介于62~161℃,和3井碳酸盐岩受到过热事件的影响,辉长岩的侵入改善了和3井碳酸盐岩的储层物性。

关 键 词:巴楚地区  辉长岩  地球化学  流体包裹体  碳酸盐岩改造
文章编号:1005-2321(2008)02-0090-10
修稿时间:2007年12月20

The characteristics of intrusive rocks and their influence on carbonate reservoir development in the Bachu area, Tarim basin
Nie Baofeng,Yu Bingsong,Zhu Jinfu.The characteristics of intrusive rocks and their influence on carbonate reservoir development in the Bachu area, Tarim basin[J].Earth Science Frontiers,2008,15(2):90-99.
Authors:Nie Baofeng  Yu Bingsong  Zhu Jinfu
Abstract:Through the microscopic identification,geochemical analysis and fluid inclusion investigation,we studied the igneous rocks from the Well He-3 in the Bachu area.The composition of gabbro in the Well He-3 shows that w(SiO2) 44.89%-45.39%,w(K2O+Na2O) 4.04%-4.67%,and w(Na2O) /w(K2O) 2.16-4.23;the rock is rich in Ba with a negative Sr anomaly;∑REE(163.43-215.99)×10-6,LREE/HREE 5.14-5.58,LaN/YbN 5.192-5.980,and δEu 0.926-1.002.The chemical characteristics and tectonic diagram show that the rock occurs in a typical within-plate environment,and belongs to the Na-rich alkaline series.Primary fluid inclusions from the carbonate in the Well He-3 nearby the gabbro intrusion have the homogenization temperature between 62 ℃ and 161 ℃.These data and the data of permeability and porosity indicate that the hydrothermal alternation has occurred in the Ordovician carbonate,which is likely to improve the reservoir quality.
Keywords:Bachu area  gabbro  geochemistry  fluid inclusions  carbonate alteration
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