羌塘盆地隆额尼-昂达尔错古油藏的白云岩组构特征及铅同位素意义
    点此下载全文
引用本文:刘建清,陈文斌,杨平,陈文西,付修根.2008.羌塘盆地隆额尼-昂达尔错古油藏的白云岩组构特征及铅同位素意义[J].地球学报,29(1):72-80.
DOI:10.3975/cagsb.2008.01.09
摘要点击次数: 5041
全文下载次数: 7127
作者单位E-mail
刘建清 成都地质矿产研究所沉积与能源地质研究室,四川成都610082 liujql@163.net 
陈文斌 成都地质矿产研究所沉积与能源地质研究室,四川成都610082  
杨平 成都地质矿产研究所沉积与能源地质研究室,四川成都610082  
陈文西 成都地质矿产研究所沉积与能源地质研究室,四川成都610082  
付修根 成都地质矿产研究所沉积与能源地质研究室,四川成都610082  
基金项目:国家油气专项(编号:XQ2004-06)
中文摘要:以系统的岩石学及沉积相分析为基础,深入探讨了隆额尼-昂达尔错古油藏白云岩及其伴生灰岩的铅同位素特征,认为该区白云岩及伴生灰岩具有统一的铅来源,铅主要来自中央隆起带变质岩、岩浆岩及再旋回沉积的三叠系地层,为地幔、造山带、地壳等多源混合的异常铅.铅元素在含量上与沉积相带关系十分明显,仍受沉积过程的控制,后期构造作用并未带入大量深部流体进行白云岩的交代作用.该区白云岩仍保存有大量具成因意义的组构信息,主要体现在:典型混合水交代成因的雾心亮边结构、等厚环边和世代生成结构、残余鲕粒结构及藻纹层构造等,该区白云岩为混合水交代成因.构造只是起到白云岩化后期的改造作用.
中文关键词:白云岩  岩石组构  铅同位素  羌塘盆地
 
The Dolomite Fabric Characteristics and Lead Isotope Significance of the Ancient Oil Accumulation in Long'eni-Angdar Lake, Qiangtang Basin
Abstract:Based on a systematic lithologic and sedimentary facies analysis,this paper deals in detail with Pb isotope characteristics of dolomite and associated limestone in the Long'eni-Angdar Co ancient oil accumulation.The dolomite and associated calcite seem to have the same Pb source,which was derived mainly from metamorphic rocks,magmatic rocks and recycled Triassic deposits in the uplift area of Qiangtang basin,thus probably being multi-source mixed anomalous lead from the mantle,the orogenic belt and the crust.The Pb content has distinctive relationship with sedimentary facies,still under the control of the sedimentary process.Late tectonic activities did not bring large quantities of hot fluids from the interior of the earth for the replacement of dolomite,and hence dolomite still preserves many typical structures of genetic significance,such as fogged center and clear margin,ring structure and generations of minerals,remnant oolitic texture and algal stromatolite.The dolomite might have resulted from mixed water replacement of calcite,and tectonic activities only exerted late alteration effects on dolomite.
keywords:dolomite  lithologic structure  Pb isotope  Qiangtang basin
查看全文  查看/发表评论  下载PDF阅读器
版权所有 《地球学报》编辑部 Copyright©2008 All Rights Reserved
主管单位:中国地质调查局 主办单位:中国地质科学院
地址: 北京市西城区百万庄大街26号,中国地质科学院东楼317室 邮编:100037 电话:010-68327396 E-mail: diqiuxb@126.com
技术支持:北京勤云科技发展有限公司
京ICP备05029128号-6

京公网安备 11010202007616号