Geology and petrography of Sabon Garin Kara and environs part of Malumfashi sheet 79 NE Nigeria

Ahmed Abubakar Sarki, M. Kwaya, Nasir Abdullahi Maiauduga, Timothy A. Adedokun, Y. Muhammad, Abubakar Nasir Karofi, A. Maigari
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引用次数: 1

Abstract

The study area is about 40 km2 that is (8 km × 5 km) which is located in Gwarzo Local Government area of Kano State part of  Malumfashi sheet 79NE which lies within Longitude E07°57’19.5” and E08°00’00” and Latitude N11° 51’30”andN11°47‘00. Major rock types identified include medium grained biotite-muscovite granite, coarse grained muscovite-biotite granites, quartz-syenite, and quartz-monzonites. Most of the crystals show subhedral to anhedral form and a perfect cleavage is somehow visible. The interference colours observed under cross-polarized light include blue, dark grey, light grey, some pinkish colour and brown colour which disappear upon the stage rotation. Albite and Carlsbad twinning are seen and used to identify the feldspars. Various structural features were observed with NE- SW trend which represents the final imprint of the Pan-African orogeny. Key words: Biotite, granite, cross-polarized, twinning.
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Sabon Garin Kara和Malumfashi sheet 79的周边地区的地质和岩石学
研究区面积约为40平方公里(8公里× 5公里),位于Malumfashi sheet 79NE的卡诺州Gwarzo地方政府区域,位于经度E07°57 ' 19.5”和E08°00 ' 00”,纬度N11°51 ' 30”和N11°47 ' 00之间。确定的主要岩石类型包括中粒黑云母-白云母花岗岩、粗粒白云母-黑云母花岗岩、石英-正长岩和石英-二长岩。多数晶体呈半面体或倒面体状,并有明显的解理。在交叉偏振光下观察到的干涉色包括蓝色、深灰色、浅灰色、一些粉红色和棕色,这些颜色在舞台旋转时消失。钠长石和卡尔斯巴德孪晶可以用来识别长石。具有NE- SW走向的各种构造特征,代表了泛非造山运动的最终印记。关键词:黑云母,花岗岩,交叉极化,孪生。
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