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Sedimentology of the Pindiga Formation, Gongola Basin, Ne-Nigeria

Abubakar Sadiq Maigari

ISBN 10: 3846519162 / ISBN 13: 9783846519165
Editorial: LAP Lambert Academic Publishing
Nuevos Condición: New Encuadernación de tapa blanda
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Descripción

Paperback. 164 pages. Dimensions: 8.7in. x 5.9in. x 0.4in.An integrated studies was conducted on the Middle Pindiga Formation (Dumbulwa, Deban Fulani and Gulani Members) involving facies analysis and clay mineralogy. Ten litho-sections were studied within the outcropping belt of the Gongola Basin, which include: Badabdi, Yayaru Daura, Nguzwa, Chole sections from Dumbulwa Member; Dampami, Sabongarin Zambuk and Deba (Borrow Pit) sections from Deban Fulani Member; and Dogon Zaga, Gulani and Maliya sections from Gulani Member. Based on facies sequences and associations, shallow marine, estuarine and braided river systems were identified as the major environments of depositions. Clay mineralogical analysis reveals that the Dumbulwa Member mudstonesclaystones are dominated by kaolinite with minor illite, while the Gulani and Deban Fulani Members are dominated mainly by kaolinite-montmorillonite and Kaolinite-montmorillonite-illite respectively as the clay mineral assemblages while quartz, feldspars and heamatite are the non-clay minerals associated with the entire sediments. Preliminary petro-physical analysis indicates that the sandy members have good reservior qualities. This item ships from multiple locations. Your book may arrive from Roseburg,OR, La Vergne,TN. N° de ref. de la librería 9783846519165

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Detalles bibliográficos

Título: Sedimentology of the Pindiga Formation, ...

Editorial: LAP Lambert Academic Publishing

Encuadernación: Paperback

Condición del libro:New

Tipo de libro: Paperback

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Sinopsis:

An integrated studies was conducted on the Middle Pindiga Formation (Dumbulwa, Deban Fulani and Gulani Members) involving facies analysis and clay mineralogy. Ten litho-sections were studied within the outcropping belt of the Gongola Basin, which include: Badabdi, Yayaru Daura, Nguzwa, Chole sections from Dumbulwa Member; Dampami, Sabongarin Zambuk and Deba (Borrow Pit) sections from Deban Fulani Member; and Dogon Zaga, Gulani and Maliya sections from Gulani Member. Based on facies sequences and associations, shallow marine, estuarine and braided river systems were identified as the major environments of depositions. Clay mineralogical analysis reveals that the Dumbulwa Member mudstones/claystones are dominated by kaolinite with minor illite, while the Gulani and Deban Fulani Members are dominated mainly by kaolinite-montmorillonite and Kaolinite-montmorillonite-illite respectively as the clay mineral assemblages while quartz, feldspars and heamatite are the non-clay minerals associated with the entire sediments. Preliminary petro-physical analysis indicates that the sandy members have good reservior qualities.

About the Author:

The author currently teaches geology at the Abubakar Tafawa Balewa University, Bauchi-Nigeria. He obtained his B.Sc. in geology from the University of Maiduguri-Nigeria in 1991. He enrolled for and successfully completed his M.Sc. and Ph.D. in Sedimentology and Petroleum Geology from the same A.T.B.U. Bauchi, in 1998 and 2011 respectively.

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