塔里木盆地奥陶系孔隙型白云岩储层成因

张静; 罗平

doi:10.11781/sysydz201005470

塔里木盆地奥陶系孔隙型白云岩储层成因

doi: 10.11781/sysydz201005470

张静,
罗平

中国石油勘探开发研究院, 提高石油采收率国家重点实验室, 北京, 100083

基金项目: 国家重点基础研究发展计划(973计划)项目(2006CB202304)

详细信息

作者简介:
张静(1979- ),女,博士,工程师,主要从事碳酸盐岩储层研究.E-mail:zj_1224@petrochina.com.cn.

中图分类号: TE122.2⁺1
计量
- 文章访问数: 3015
- HTML全文浏览量: 53
- PDF下载量: 900
- 被引次数: 0
出版历程
- 收稿日期: 2010-03-12
- 修回日期: 2010-09-28
- 刊出日期: 2010-10-28

GENESIS OF ORDOVICIAN MATRIX-POROSITY DOLOMITE RESERVOIR IN THE TARIM BASIN

State Key Laboratory of Enhanced Oil Recovery, Research Institute of Petroleum Exploration and Development, CNPC, Beijing 100083, China

摘要

摘要: 塔里木盆地下奥陶统存在大量基质孔隙发育的深埋白云岩,是一类优质储层。岩心、薄片观察和阴极发光分析表明该类白云岩的发育具有明显的相控特征,以滩相颗粒灰岩为原岩。岩石学特征和微量元素、有序度及包裹体均一温度特征研究表明,该类白云岩形成于埋藏环境中,属埋藏白云石化作用的产物。由微量元素、稀土元素及锶同位素特征判断白云石化流体为受改造的海水,很可能与深部封存的蒸发台地相海水有关。推断塔里木盆地二叠纪大规模火山活动是台地相区白云石化作用的主要驱动机制,寒武系蒸发台地中富含镁离子的海水在广泛的热作用驱动下交代其上覆灰岩而形成白云岩。
- 白云石化 /
- 白云岩 /
- 储层 /
- 下奥陶统 /
- 塔里木盆地
Abstract: There is a large quantity of deeply buried dolomite with well-developed matrix porosity in the Lower Ordovician of the Tarim Basin which can be quality reservoir.The development of this kind of dolomite is facies-controlled and the initial rock is grainstone of grain bank facies,according to the analyses of cores,thin sections and cathodeluminescence.The dolomite formed under burial condition which is the product of burial dolomitization,based on the study of petrology,trace element,degree of order and homogenization temperature of the dolomite.It is predicted from the trace element,rare earth element and Sr isotope that the dolomitizing fluid is modified seawater which may be related to Mg²⁺-bearing seawater in Cambrian evaporative platform.Permian volcanic activity is supposed to be the driving force of dolomitization over the entire platform and the burial dolomite in the Lower Ordovician formed by means of the replacement of overlying limestone by underlying Mg²⁺-bearing seawater in Cambrian evaporative platform through thermal convection.
- dolomitization /
- dolomite /
- reservoir /
- Lower Ordovician /
- Tarim Basin

HTML全文

参考文献(11)

[1]	冯增昭,鲍志东,吴茂炳,等.塔里木地区奥陶纪岩相古地理[J].古地理学报,2007,9(5):447-460.
[2]	冯增昭,鲍志东,吴茂炳,等.塔里木地区寒武纪和奥陶纪岩相古地理[M].北京:地质出版社,2005.
[3]	何宏,彭苏萍,邵龙义,等.巴楚隆起与阿瓦提凹陷寒武系及奥陶系沉积古地理分析[J].煤田地质与勘探,2002,30(6):1-4.
[4]	高志前,王惠民,樊太亮,等.塔里木盆地寒武-奥陶系沉积相、沉积体系及其组合序列[J].新疆石油天然气,2005,1(1):30-35.
[5]	黄文辉,杨敏,于炳松,等.塔中地区寒武系-奥陶系碳酸盐岩Sr元素和Sr同位素特征[J].地球科学--中国地质大学学报,2006,31(6):839-845.
[6]	强子同.碳酸盐岩储层地质学[M].北京:石油大学出版社,1995.
[7]	曾理,万茂霞,彭英.白云石有序度及其在石油地质中的应用[J].天然气勘探与开发,2004,27(4):64-67.
[8]	刘英俊.元素地球化学导论[M].北京:地质出版社,1987.
[9]	李伟,蒲仁海,卿海若.威林斯頓盆地奥陶系白云岩储层同位素与成岩作用分析[J].石油实验地质,2009,31(1):87-91.
[10]	ALLEN J R,MATTHESS R K.Isotope signatures associated with early meteoric diagenesis[J].Sedimentology,1982,29:797-817.
[11]	康玉柱.新疆两大盆地石炭-二叠系火山岩特征与油气[J].石油实验地质,2008,30(4):321-327.