Please use this identifier to cite or link to this item: http://ir.futminna.edu.ng:8080/jspui/handle/123456789/4780
Title: DELTAIC AND SHELF DEPOSITIONAL PACKAGES OF THE GULANI MEMBER OF PINDIGA FORMATION, GONGOLA SUB-BASIN, NORTHERN BENUE TROUGH, N.E. NIGERIA
Authors: Shettima, B
Goro, A I
Bukar, M
Mohammed, Y B
Keywords: Gongola Sub-Basin
Gulani Member
Deba Fulani Member
Issue Date: Apr-2018
Publisher: International Journal of Research Granthaalayah
Series/Report no.: Vol.6 (Iss.4): 188-197;
Abstract: Stratigraphic and facies analysis of the Gulani Member of the Pindiga Formation in the Gongola Sub-basin of the Northern Benue Trough indicated that the lithostratigraphic architecture of the formation are characterized by three bioturbated lithologic units. These includes the lower succession of heterolithic units with fine grained sandstones and mudstone interbeds, passing into succession of medium-coarse grained sandstone with dominantly trough crossbeds and a upper succession of medium grained trough crossbedded sandstone and mudstone interbeds. Facies evaluation of these distinct succession indicated development of a corresponding pro-delta sands and clays, moving into delta front sands and then shelf sandstone and claystone respectively. Thus suggesting that the Gulani Member was generally formed in a coastal setting defined by river dominated deltaic setting and shelf depositional environment
URI: http://repository.futminna.edu.ng:8080/jspui/handle/123456789/4780
ISSN: ISSN- 2350-0530(O), ISSN- 2394-3629(P)
Appears in Collections:Geology

Files in This Item:
File Description SizeFormat 
shettima et al 2018 19_IJRG18_A04_1320.pdf592.65 kBAdobe PDFView/Open


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.