Stable Isotope Characteristics of Akiri Vein Copper Mineralization, Nasarawa, Nigeria

The Akiri vein copper mineralization was investigated for its carbon and oxygen isotopic composition to determine the characteristics of the mineralizing fluid. Carbon and oxygen isotope analyses of Akiri siderite range between δ13C values (-1.05 to -1.71‰) and δ13O values (-14.94 to -15.18) respect...

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Main Authors: IO Folorunso, RB Bale, JID Adekeye
Format: Article
Language:English
Published: Joint Coordination Centre of the World Bank assisted National Agricultural Research Programme (NARP) 2015-07-01
Series:Journal of Applied Sciences and Environmental Management
Online Access:https://www.ajol.info/index.php/jasem/article/view/119951
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author IO Folorunso
RB Bale
JID Adekeye
author_facet IO Folorunso
RB Bale
JID Adekeye
author_sort IO Folorunso
collection DOAJ
description The Akiri vein copper mineralization was investigated for its carbon and oxygen isotopic composition to determine the characteristics of the mineralizing fluid. Carbon and oxygen isotope analyses of Akiri siderite range between δ13C values (-1.05 to -1.71‰) and δ13O values (-14.94 to -15.18) respectively. δ 13C isotopic composition is comparable to values expected for Cretaceous marine carbonates. The 18O depletion in the vein siderite indicates dominant meteoric water sources involved for carbonates precipitation. This significant depletion between the δ18O compositions of Akiri siderite compared with carbonates from other parts of the basin probably indicate differential formational temperature or fluid composition.
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spelling doaj.art-7ec87e43335a4beba282b0d1959cb1392024-04-22T19:47:04ZengJoint Coordination Centre of the World Bank assisted National Agricultural Research Programme (NARP)Journal of Applied Sciences and Environmental Management2659-15022659-14992015-07-01192Stable Isotope Characteristics of Akiri Vein Copper Mineralization, Nasarawa, NigeriaIO FolorunsoRB BaleJID AdekeyeThe Akiri vein copper mineralization was investigated for its carbon and oxygen isotopic composition to determine the characteristics of the mineralizing fluid. Carbon and oxygen isotope analyses of Akiri siderite range between δ13C values (-1.05 to -1.71‰) and δ13O values (-14.94 to -15.18) respectively. δ 13C isotopic composition is comparable to values expected for Cretaceous marine carbonates. The 18O depletion in the vein siderite indicates dominant meteoric water sources involved for carbonates precipitation. This significant depletion between the δ18O compositions of Akiri siderite compared with carbonates from other parts of the basin probably indicate differential formational temperature or fluid composition.https://www.ajol.info/index.php/jasem/article/view/119951
spellingShingle IO Folorunso
RB Bale
JID Adekeye
Stable Isotope Characteristics of Akiri Vein Copper Mineralization, Nasarawa, Nigeria
Journal of Applied Sciences and Environmental Management
title Stable Isotope Characteristics of Akiri Vein Copper Mineralization, Nasarawa, Nigeria
title_full Stable Isotope Characteristics of Akiri Vein Copper Mineralization, Nasarawa, Nigeria
title_fullStr Stable Isotope Characteristics of Akiri Vein Copper Mineralization, Nasarawa, Nigeria
title_full_unstemmed Stable Isotope Characteristics of Akiri Vein Copper Mineralization, Nasarawa, Nigeria
title_short Stable Isotope Characteristics of Akiri Vein Copper Mineralization, Nasarawa, Nigeria
title_sort stable isotope characteristics of akiri vein copper mineralization nasarawa nigeria
url https://www.ajol.info/index.php/jasem/article/view/119951
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AT rbbale stableisotopecharacteristicsofakiriveincoppermineralizationnasarawanigeria
AT jidadekeye stableisotopecharacteristicsofakiriveincoppermineralizationnasarawanigeria