尼日利亚贝努埃海槽北部约拉亚盆地白垩系Jessu组沉积相分析及古环境

M. Usman, Y. Mamman, B. Yandoka, Abubakar S. Mohammed, Binan Bulus, U. Abubakar, A. Bello
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引用次数: 0

摘要

杰苏组是尼日利亚东北部贝努埃海槽北部约拉亚盆地的海相白垩纪沉积之一。对Dukul和Cham河露头处的Jessu组进行了岩相研究,以确定相,建立相组合,重建古沉积环境。根据岩性、粒度、沉积构造和生物扰动程度,确定了10个相。这些相形成4个相组,分别为FA-1(近海)、FA-2(下滨面)、FA-3(中滨面)和FA-4(上滨面)。这些相组合形成了由近海海相向滨面向上粗化的单元,表明杰苏组为滨面沉积。向上粗化的相序表明风暴和波浪对海岸系统的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Facies analysis and paleoenvironment of deposition of Cretaceous Jessu Formation, Yola Sub-basin, Northern Benue Trough, Nigeria
The Jessu Formation is one of the marine Cretaceous sediments in the Yola Sub-basin of the Northern Benue Trough, NE Nigeria. Lithofacies studies was carried out on the Jessu Formation exposed at Dukul and Cham streams outcrops, in order to identify facies, establish facies association and re-construct the paleodepositional environment. Ten (10) facies were identified on the bases of lithology, grain size, sedimentary structures and degree of bioturbation. These facies form four (4) facies associations, namely: the FA-1 (offshore marine), FA-2 (lower shoreface), FA-3 (middle shoreface) and FA-4 (upper shoreface). These facies associations form coarsening upward units from offshore marine to shoreface which suggests a shoreface deposit for the Jessu Formation. The coarsening upward facies succession indicated storm and wave influenced coastal system.
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