Diamonds from the Coromandel Area, West Minas Gerais State, Brazil: an update and new data on surface sources and origin

Important diamond deposits southeast of Coromandel and the local geology have been studied in an attempt to understand what surface source provided the stones. River gravels of Pleistocene to Recent age from this region have supplied most of Brazil's large diamonds over 100 ct. The upper cretac...

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Main Authors: Joachim Karfunkel, Donald Hoover, Augusto Fonseca Fernandes, Geraldo Norberto Chaves Sgarbi, Klaus Kambrock, Gustavo Diniz Oliveira
Format: Article
Language:English
Published: Sociedade Brasileira de Geologia
Series:Brazilian Journal of Geology
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892014000100325&lng=en&tlng=en
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author Joachim Karfunkel
Donald Hoover
Augusto Fonseca Fernandes
Geraldo Norberto Chaves Sgarbi
Klaus Kambrock
Gustavo Diniz Oliveira
author_facet Joachim Karfunkel
Donald Hoover
Augusto Fonseca Fernandes
Geraldo Norberto Chaves Sgarbi
Klaus Kambrock
Gustavo Diniz Oliveira
author_sort Joachim Karfunkel
collection DOAJ
description Important diamond deposits southeast of Coromandel and the local geology have been studied in an attempt to understand what surface source provided the stones. River gravels of Pleistocene to Recent age from this region have supplied most of Brazil's large diamonds over 100 ct. The upper cretaceous Capacete Formation of the Mata da Corda Group, composed of mafic volcanoclastic, pyroclastic and epiclastic material, has been worked locally for diamonds, nevertheless considered non-economic. The authors present results of their study of a deactivated small mine, representing the first report with description and analyses of two gem diamonds washed from this material. Hundreds of kimberlites, discovered in the last half century in the region, are sterile or non-economic. We propose that the surface source of the diamonds is the Capacete "conglomerado". The volume of this material is enormous representing a potential resource for large-scale mining. The authors suggest detailed studies of the volcanic facies of this unit focusing on the genesis, distribution and diamond content. As to the question concerning the origin of these diamondiferous pyroclastic rocks, the authors exclude the kimberlites and point towards the large Serra Negra and Salitre alkaline complexes which are considered the primary source for the pyroclastic units of the Mata da Corda Group. They propose that early eruptive phases of this alkaline complex brought diamonds from a mantle source to the surface, much as happens with traditional kimberlites, to explain the association of such huge carbonatite complexes and diamonds.
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spelling doaj.art-4f5b95dfb9c2428e954639a0bb1b3c6f2022-12-22T03:36:28ZengSociedade Brasileira de GeologiaBrazilian Journal of Geology2317-469244232533810.5327/Z2317-4889201400020011S2317-48892014000100325Diamonds from the Coromandel Area, West Minas Gerais State, Brazil: an update and new data on surface sources and originJoachim KarfunkelDonald HooverAugusto Fonseca FernandesGeraldo Norberto Chaves SgarbiKlaus KambrockGustavo Diniz OliveiraImportant diamond deposits southeast of Coromandel and the local geology have been studied in an attempt to understand what surface source provided the stones. River gravels of Pleistocene to Recent age from this region have supplied most of Brazil's large diamonds over 100 ct. The upper cretaceous Capacete Formation of the Mata da Corda Group, composed of mafic volcanoclastic, pyroclastic and epiclastic material, has been worked locally for diamonds, nevertheless considered non-economic. The authors present results of their study of a deactivated small mine, representing the first report with description and analyses of two gem diamonds washed from this material. Hundreds of kimberlites, discovered in the last half century in the region, are sterile or non-economic. We propose that the surface source of the diamonds is the Capacete "conglomerado". The volume of this material is enormous representing a potential resource for large-scale mining. The authors suggest detailed studies of the volcanic facies of this unit focusing on the genesis, distribution and diamond content. As to the question concerning the origin of these diamondiferous pyroclastic rocks, the authors exclude the kimberlites and point towards the large Serra Negra and Salitre alkaline complexes which are considered the primary source for the pyroclastic units of the Mata da Corda Group. They propose that early eruptive phases of this alkaline complex brought diamonds from a mantle source to the surface, much as happens with traditional kimberlites, to explain the association of such huge carbonatite complexes and diamonds.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892014000100325&lng=en&tlng=enDiamantesCoromandelorigem
spellingShingle Joachim Karfunkel
Donald Hoover
Augusto Fonseca Fernandes
Geraldo Norberto Chaves Sgarbi
Klaus Kambrock
Gustavo Diniz Oliveira
Diamonds from the Coromandel Area, West Minas Gerais State, Brazil: an update and new data on surface sources and origin
Brazilian Journal of Geology
Diamantes
Coromandel
origem
title Diamonds from the Coromandel Area, West Minas Gerais State, Brazil: an update and new data on surface sources and origin
title_full Diamonds from the Coromandel Area, West Minas Gerais State, Brazil: an update and new data on surface sources and origin
title_fullStr Diamonds from the Coromandel Area, West Minas Gerais State, Brazil: an update and new data on surface sources and origin
title_full_unstemmed Diamonds from the Coromandel Area, West Minas Gerais State, Brazil: an update and new data on surface sources and origin
title_short Diamonds from the Coromandel Area, West Minas Gerais State, Brazil: an update and new data on surface sources and origin
title_sort diamonds from the coromandel area west minas gerais state brazil an update and new data on surface sources and origin
topic Diamantes
Coromandel
origem
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892014000100325&lng=en&tlng=en
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