Heavy mineral analysis of Eocene sands and sandstones of Nanka Formation, Cenozoic Niger Delta petroleum province

The heavy minerals present in lithologic sand and sandstone units of Nanka Formation are mainly zircon, rutile, tourmaline, apatite, staurolite, and opaque minerals (Goethite, hematite, ilmenite), which are present dominant in weathered sandstones when analysed using petrographic varietal studies to...

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Main Authors: Osuwake Omini Etimita, Francis Thomas Beka
Format: Article
Language:English
Published: Taylor & Francis Group 2020-10-01
Series:Geology, Ecology, and Landscapes
Subjects:
Online Access:http://dx.doi.org/10.1080/24749508.2019.1633218
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author Osuwake Omini Etimita
Francis Thomas Beka
author_facet Osuwake Omini Etimita
Francis Thomas Beka
author_sort Osuwake Omini Etimita
collection DOAJ
description The heavy minerals present in lithologic sand and sandstone units of Nanka Formation are mainly zircon, rutile, tourmaline, apatite, staurolite, and opaque minerals (Goethite, hematite, ilmenite), which are present dominant in weathered sandstones when analysed using petrographic varietal studies to infer provenance, diagenesis and source area weathering history. The low-diversity and relative abundance of heavy mineral assemblages are controlled by provenance and diagenetic processes, and these present limitations in accurate reconstruction of the paleo-history of these lithologic units using heavy minerals analysis alone. These lithologic Eocene units are derived from intensely weathered granitic and metamorphic source rocks and they are composed dominantly of matured polycyclic sediments.
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spelling doaj.art-7dc584eefd1b4413a27d2e4a79bb84a02022-12-21T23:21:17ZengTaylor & Francis GroupGeology, Ecology, and Landscapes2474-95082020-10-014425125610.1080/24749508.2019.16332181633218Heavy mineral analysis of Eocene sands and sandstones of Nanka Formation, Cenozoic Niger Delta petroleum provinceOsuwake Omini Etimita0Francis Thomas Beka1University of Port HarcourtUniversity of Port HarcourtThe heavy minerals present in lithologic sand and sandstone units of Nanka Formation are mainly zircon, rutile, tourmaline, apatite, staurolite, and opaque minerals (Goethite, hematite, ilmenite), which are present dominant in weathered sandstones when analysed using petrographic varietal studies to infer provenance, diagenesis and source area weathering history. The low-diversity and relative abundance of heavy mineral assemblages are controlled by provenance and diagenetic processes, and these present limitations in accurate reconstruction of the paleo-history of these lithologic units using heavy minerals analysis alone. These lithologic Eocene units are derived from intensely weathered granitic and metamorphic source rocks and they are composed dominantly of matured polycyclic sediments.http://dx.doi.org/10.1080/24749508.2019.1633218heavy mineraldiagenesisprovenanceweatheringtransportationmineral assemblages
spellingShingle Osuwake Omini Etimita
Francis Thomas Beka
Heavy mineral analysis of Eocene sands and sandstones of Nanka Formation, Cenozoic Niger Delta petroleum province
Geology, Ecology, and Landscapes
heavy mineral
diagenesis
provenance
weathering
transportation
mineral assemblages
title Heavy mineral analysis of Eocene sands and sandstones of Nanka Formation, Cenozoic Niger Delta petroleum province
title_full Heavy mineral analysis of Eocene sands and sandstones of Nanka Formation, Cenozoic Niger Delta petroleum province
title_fullStr Heavy mineral analysis of Eocene sands and sandstones of Nanka Formation, Cenozoic Niger Delta petroleum province
title_full_unstemmed Heavy mineral analysis of Eocene sands and sandstones of Nanka Formation, Cenozoic Niger Delta petroleum province
title_short Heavy mineral analysis of Eocene sands and sandstones of Nanka Formation, Cenozoic Niger Delta petroleum province
title_sort heavy mineral analysis of eocene sands and sandstones of nanka formation cenozoic niger delta petroleum province
topic heavy mineral
diagenesis
provenance
weathering
transportation
mineral assemblages
url http://dx.doi.org/10.1080/24749508.2019.1633218
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