乍得Bongor盆地基底岩性特征及形成时代
Basement Lithology Characteristics and Forming Age of Bongor Basin Chad
DOI: 10.12677/OJNS.2016.41009, PDF, HTML, XML,  被引量 下载: 2,374  浏览: 6,856  国家科技经费支持
作者: 张明瑜, 田志彬, 王 奇:中油长城钻探工程有限公司,辽宁 盘锦;宋柏荣, 施玉华:中油辽河油田分公司,辽宁 盘锦;张乃丹:长江大学,湖北 武汉
关键词: 乍得Bongor盆地基底变质岩岩浆岩锆石U-Pb年龄Chad Bongor Basin Basement Metamorphic Rocks Magmatic Rocks Zircon U-Pb Age
摘要: 乍得Bongor盆地基底为早寒武世之前形成的一套结晶基岩,该套岩石富含油气,因此,对盆地基底岩石类型及形成时代的研究越显重要。本文主要以岩心观察、描述为基础,采用岩石薄片鉴定、单颗粒锆石U-Pb同位素测定等方法,对乍得Bongor盆地基底岩性进行鉴定和划分,并对其形成和演化时代进行分析。结果认为:岩性为由变质岩和岩浆岩组成的杂岩体,岩性包括2大类14个亚类;单锆石测年年龄集中在550~600 Ma,变质岩原岩年龄主要集中在616 ± 6~526.5 ± 2.7 Ma,最老的原岩年龄1006 ± 12~946 ± 5 Ma,变质年龄在553 ± 19~464 ± 5 Ma,岩浆岩的年龄主要集中在621 ± 16~525.3 ± 2.5 Ma。由于岩石类型、性质及形成时代的差异,造成后期地质作用改造和储层的发育程度不同。
Abstract: The basement of the Bongor basin Chad is formed by a set of crystalline basement rocks before the Early Cambrian, which is rich in oil and gas. Therefore, it is more important to study the type of basement rocks and the formation age of the basin. This paper is mainly based on the core observation and description, by identification of rock slice, single grain zircon U-Pb isotope determination, Chad Bongor basin’s basement lithology of identification and delineation, and the formation and evolution of era were analyzed. The results show that the lithology is composed of metamorphic rocks and magmatic rocks, which are composed of 14 kinds of 2 sub categories; Single Zircon dating was concentrated in the age of 550 - 600 Ma, the age of metamorphic rocks was mainly con- centrated in 616 ± 6 - 526.5 ± 2.7 Ma, the oldest old rock age was 1006 ± 12 - 946 ± 5 Ma, metamorphic age was 553 ± 19 - 464 ± 5 Ma, the age of magmatic rock was mainly concentrated in 621 ± 16 - 525.3 ± 2.5 Ma. Because of the difference of the rock type, nature and the age of formation, the transformation of the geological function and the development of the reservoir are different in the later stage.
文章引用:张明瑜, 宋柏荣, 田志彬, 张乃丹, 施玉华, 王奇. 乍得Bongor盆地基底岩性特征及形成时代[J]. 自然科学, 2016, 4(1): 63-80. http://dx.doi.org/10.12677/OJNS.2016.41009

参考文献

[1] 陆松年. 初论“泛华夏造山作用”与加里东和泛非造山作用的对比[J]. 地质通报, 2004, 23(9-10): 952-957.
[2] 史玉玲, 侯读杰, 窦立荣, 等. 乍得Bongor盆地原油母质生源特征[J]. 石油地质与工程, 2011, 25(1): 5-9.
[3] 宋红日, 窦立荣, 肖坤叶, 等. Bongor盆地油气成藏地质条件及分布规律初探[J]. 石油与天然气地质, 2009, 30(6): 762-767.
[4] 窦立荣, 肖坤叶, 胡勇, 等. 乍得Bongor盆地石油地质特征及成藏模式[J]. 石油学报, 2011, 32(3): 379-386.
[5] 李德威, 廖群安, 袁晏明, 等. 喜马拉雅中段日玛那麻粒岩锆石U-Pb年代学[J]. 科学通报, 2003, 48(20): 2176- 2179.
[6] 吴福元, 孙德有, 李惠民, 等. 松辽盆地基底岩石的锆石U-Pb年龄[J]. 科学通报, 2000, 45(6): 656-660.
[7] 姜丽萍, 柴风梅, 杨富圈, 等. 新疆阿尔泰两棵树铁矿区二长花岗岩LA-ICP-MS锆石定年及地质意义[J]. 现代地质, 2011, 25(4): 712-719.
[8] 陈高潮, 魏仙样, 忤康林, 等. 内蒙古西部阿拉善右旗下石炭统白山组碎屑岩锆石LA-ICP-MS U-Pb测年及意义[J]. 地质通报, 2011, 30(6): 955-961.
[9] 修群业, 殷艳杰, 等. 单锆石定年样品的采集及矿物分选[J]. 前寒武纪研究进展, 2001, 24(2): 107-109.
[10] Yuan, H.L., Gao, S., Liu, X.M., Li, H.M., Günther, D. and Wu, F.Y. (2004) Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry. Geostandards and Geo- analytical Research, 28, 353-370.
http://dx.doi.org/10.1111/j.1751-908X.2004.tb00755.x
[11] 吴元保, 郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报, 2004, 49(16): 1589-1604.
[12] 钱一雄, 何治亮, 蔡习尧, 等. 塔中地区上泥盆统东河砂岩和志留系砂岩的锆石特征、SHRIMP U-Pb年龄及地质意义[J]. 石油学报, 2007, 23(11): 3003-3014.
[13] Hermann, J., Rubatto, D. and Korsakov, A. (2001) Multiple Zircon Growth during Fast Exhumation of Diamondiferous, Deeply Subducted Continental Crust (Kokchetav Massif, Kazakhstan). Contributions to Mineralogy and Petrology, 141, 66-82.
http://dx.doi.org/10.1007/s004100000218
[14] 唐俊华, 顾连兴, 张尊忠, 等. 咸水泉片麻状花岗岩锆石热液增边阴极发光及稀土元素特征[J]. 自然科学进展, 2008, 18(7): 769-777.