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LITHOSTRATIGRAPHY OF NIGERIA AN-OVERVIEW

机译:尼日利亚岩性地层概况

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Nigeria lies very close to the equator (hot country) West coast Africa between latitude 4 N and 14 N degree and longitude 2 E and 15 E degree. The country is located at the Northern end of Eastern branch of west coast of Africa rift system. Nigeria geological set up comprises broadly sedimentary formation and crystalline basement complex, which occur more or less in equal proportion all over the country. The sediment is mainly Upper Cretaceous to recent in age while the basement complex rocks are thought to be Precambrian. The studied area lies between latitude 12.4" and 11.11"W and longitude 13.81" and 14.13" S. The studied area is underlain by Precambrian basement complex of southern western Nigeria .The major rock in the area is charnokite and granite rock. The granite rock which are member of the older granite suite occupy about 65% of the total area .The principal granite is petrographic variety are recognized .The fine grained biotite-granite medium-coarse, non porphyritic biotite -hornblende granite and coarse-porphyritic biotite -hornblende granite. Also three main textural type of Charnokitic rock are also distinguished are coarse grained, massive fine grained and gneissic fine grained .The mode of occurrence of rock is three (1) core of the granite rock as exemplified by study area and few smaller bodies (2) Margin of the granite bodies as seen in Ijare and Uro edemo-idemo Charnokitic bodies and (3) Discrete bodies of the gneissic fine grained Charnokitic rock within the country gneisses as seen in Ilaro and Iju and Emirin village. All the charnokite in the region are dark-greenish to greenish-gray rocks with bluish quartz and greenish feldspar.
机译:尼日利亚非常靠近赤道(炎热的国家)西海岸非洲,纬度4 N和14 N,经度2 E和15E。该国位于非洲西海岸裂谷系统东部分支的北端。尼日利亚的地质构造包括广泛的沉积层和晶体基底复合体,它们在全国范围内或多或少地以相等的比例发生。沉积物主要是上白垩统至近代,而基底复杂的岩石被认为是前寒武纪的。研究区域位于纬度12.4“和11.11” W之间,经度13.81“和14.13” S之间。研究区域位于尼日利亚南部南部的前寒武纪基底复合体之下。该区域的主要岩石是黑钙石和花岗岩。属于较老花岗岩组的花岗岩岩石约占总面积的65%。主要花岗岩是岩相变种。细粒黑云母-花岗岩中粗,非斑状黑云母-角闪石花岗岩和粗斑状黑云母-角闪石花岗岩。查诺基质岩的三种主要构造类型也分别是粗粒状,块状细粒状和片麻质细粒状。岩石的形成方式是花岗岩的三(1)个岩心,以研究区域和较小的小块体为例(2 )在Ijare和Uro edemo-idemo Charnokitic岩体中发现的花岗岩体的边缘,以及(3)在Ilaro和Iju和Emirin村中发现的乡村片麻岩中的片麻岩细粒Charnokitic岩石的离散体。该地区所有的黑钙石都是深绿色至绿色至灰色的岩石,带有蓝色的石英和绿色的长石。

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