Diamonds from Borrachudo river, São Francisco basin (Tiros, MG): morphologic and dissolution aspects

A representative set of diamonds from the Borrachudo River (114 stones) was described for the first time as to their physical characteristics, among them weight, morphology, dissolution figures, and abrasion. Most samples are low in weight (~51% less than 0.30 ct) and only ~3.5% are above 3.0 ct. However, considering the total weight, ~47% of it is concentrated in the range above 3 ct. On the other hand, there even occur diamonds with dozen of carats. The most common crystallographic forms are originated from the octahedral form by dissolution, although irregular shapes like chips and flats also occur. The diamonds show differences in form compared to their weight ranges; those up to 0.30 ct have various shapes; in the range of 0.31 to 1 ct the most common are octahedral forms and their descendants; and in stones larger than 1 ct chips and flats predominate. The general habitus of the crystals, identified by their final tetrahexahedroid shapes, chips and flats, corroborated by the dissolution figures, indicate that the diamond were submitted to strong dissolution in a magmatic environment. Residual hillocks and holes represent the final stage of dissolution. The study indicates that the abrasion by the fluvial transport was not expressive enough to cause mechanical wear, thus ca. 97% shows no sign of wear. This fact suggests a proximal source for most of these diamonds.

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Main Authors: Borges,Luis Alberto de Deus, Chaves,Mario Luiz de Sá Carneiro, Karfunkel,Joachim
Format: Digital revista
Language:English
Published: Escola de Minas 2014
Online Access:http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0370-44672014000200005
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spelling oai:scielo:S0370-446720140002000052014-07-25Diamonds from Borrachudo river, São Francisco basin (Tiros, MG): morphologic and dissolution aspectsBorges,Luis Alberto de DeusChaves,Mario Luiz de Sá CarneiroKarfunkel,Joachim Diamond Borrachudo River São Francisco Basin A representative set of diamonds from the Borrachudo River (114 stones) was described for the first time as to their physical characteristics, among them weight, morphology, dissolution figures, and abrasion. Most samples are low in weight (~51% less than 0.30 ct) and only ~3.5% are above 3.0 ct. However, considering the total weight, ~47% of it is concentrated in the range above 3 ct. On the other hand, there even occur diamonds with dozen of carats. The most common crystallographic forms are originated from the octahedral form by dissolution, although irregular shapes like chips and flats also occur. The diamonds show differences in form compared to their weight ranges; those up to 0.30 ct have various shapes; in the range of 0.31 to 1 ct the most common are octahedral forms and their descendants; and in stones larger than 1 ct chips and flats predominate. The general habitus of the crystals, identified by their final tetrahexahedroid shapes, chips and flats, corroborated by the dissolution figures, indicate that the diamond were submitted to strong dissolution in a magmatic environment. Residual hillocks and holes represent the final stage of dissolution. The study indicates that the abrasion by the fluvial transport was not expressive enough to cause mechanical wear, thus ca. 97% shows no sign of wear. This fact suggests a proximal source for most of these diamonds.info:eu-repo/semantics/openAccessEscola de MinasRem: Revista Escola de Minas v.67 n.2 20142014-06-01info:eu-repo/semantics/articletext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0370-44672014000200005en10.1590/S0370-44672014000200005
institution SCIELO
collection OJS
country Brasil
countrycode BR
component Revista
access En linea
databasecode rev-scielo-br
tag revista
region America del Sur
libraryname SciELO
language English
format Digital
author Borges,Luis Alberto de Deus
Chaves,Mario Luiz de Sá Carneiro
Karfunkel,Joachim
spellingShingle Borges,Luis Alberto de Deus
Chaves,Mario Luiz de Sá Carneiro
Karfunkel,Joachim
Diamonds from Borrachudo river, São Francisco basin (Tiros, MG): morphologic and dissolution aspects
author_facet Borges,Luis Alberto de Deus
Chaves,Mario Luiz de Sá Carneiro
Karfunkel,Joachim
author_sort Borges,Luis Alberto de Deus
title Diamonds from Borrachudo river, São Francisco basin (Tiros, MG): morphologic and dissolution aspects
title_short Diamonds from Borrachudo river, São Francisco basin (Tiros, MG): morphologic and dissolution aspects
title_full Diamonds from Borrachudo river, São Francisco basin (Tiros, MG): morphologic and dissolution aspects
title_fullStr Diamonds from Borrachudo river, São Francisco basin (Tiros, MG): morphologic and dissolution aspects
title_full_unstemmed Diamonds from Borrachudo river, São Francisco basin (Tiros, MG): morphologic and dissolution aspects
title_sort diamonds from borrachudo river, são francisco basin (tiros, mg): morphologic and dissolution aspects
description A representative set of diamonds from the Borrachudo River (114 stones) was described for the first time as to their physical characteristics, among them weight, morphology, dissolution figures, and abrasion. Most samples are low in weight (~51% less than 0.30 ct) and only ~3.5% are above 3.0 ct. However, considering the total weight, ~47% of it is concentrated in the range above 3 ct. On the other hand, there even occur diamonds with dozen of carats. The most common crystallographic forms are originated from the octahedral form by dissolution, although irregular shapes like chips and flats also occur. The diamonds show differences in form compared to their weight ranges; those up to 0.30 ct have various shapes; in the range of 0.31 to 1 ct the most common are octahedral forms and their descendants; and in stones larger than 1 ct chips and flats predominate. The general habitus of the crystals, identified by their final tetrahexahedroid shapes, chips and flats, corroborated by the dissolution figures, indicate that the diamond were submitted to strong dissolution in a magmatic environment. Residual hillocks and holes represent the final stage of dissolution. The study indicates that the abrasion by the fluvial transport was not expressive enough to cause mechanical wear, thus ca. 97% shows no sign of wear. This fact suggests a proximal source for most of these diamonds.
publisher Escola de Minas
publishDate 2014
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0370-44672014000200005
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