Sedimentary Structures and Petrography of Rocks within Akpoha Area of the Afikpo Basin Southeastern Nigeria; Constraints on Provenance

Modestus Chijioke Ohaegbulem, O. P. Aghamelu, Uwem Bassey Abia, Nonyelum Stella Iloanya
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Abstract

Sedimentary structures and petrographic studies of Akpoha area in Afikpo/Abakiliki basin  was undertaken in an attempt to understudy and determining constraints  in depositional processes in the area . The major outcrops in the area are alternating succession of sandstones and shales striking in a NE-SW direction primarily as a result of folding due to past orogeny in the area. The sandstone outcrops at Akpoha are highly indurated due to age, compaction and tectonism and occur in ridges within the shale unit. The studied shale outcrops were poorly laminated and low in fossil content.Sedimentary structures identified include;Wavy/ripple lamination, Mud cracks, Parallel lamination and Fissility.The results of the petrographic modal analysis from thin section studies show that  the sandstone consists predominantly of quartz (55 - 64%); feldspar (22 - 30%) and rock fragment (1 – 9%). The sandstones were immature, poorly to moderately sorted with angular to sub-angular grain shapes which gives clear indication of high energy of sediment deposition and short transport history from provenance.The abundance of well preserved sedimentary structures  is an indication of prolong calmness of tectonic/orogenic activities in the area. The fissility observed in shale outcrops and the high induration of the Akpoha sandstones was as a result of compaction from overburden pressure before uplift and exposure.
尼日利亚东南部阿菲克波盆地阿克波哈地区岩石的沉积结构和岩相学;对产状的制约因素
对阿菲克波/阿巴基利基盆地的阿克波哈地区进行了沉积结构和岩石学研究,试图了解和确定该地区沉积过程的制约因素。该地区的主要露头是砂岩和页岩的交替演替,呈东北-西南走向,这主要是该地区过去造山运动造成的褶皱的结果。阿克波哈的砂岩露头由于年代久远、压实和构造作用而高度硬化,并出现在页岩单元内的山脊上。所研究的页岩露头层理较差,化石含量较低。所发现的沉积结构包括:波浪形/褶皱层理、泥质裂缝、平行层理和裂隙。薄片研究的岩相模式分析结果显示,砂岩主要由石英(55-64%)、长石(22-30%)和岩石碎片(1-9%)组成。这些砂岩尚未成熟,分选程度较差至中等,颗粒形状为角形至次角形,这清楚地表明沉积物沉积的能量很高,而且从产地开始的搬运历史很短。在页岩露头中观察到的裂隙和阿克波哈砂岩的高压痕是在隆起和暴露之前由于覆盖层压力而压实的结果。
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