Diamonds from the Santo Antônio River (Delfinópolis, Minas Gerais): probable relationship with the Canastra-3 Kimberlite Article Swipe
YOU?
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· 2019
· Open Access
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· DOI: https://doi.org/10.1590/0370-44672018730051
The study identifies the Canastra-3 Kimberlite magnetic anomaly as the likely primary source of the alluvial diamonds recovered by "garimpeiros" in the Santo Antônio River basin (Delfinópolis, southwestern Minas Gerais). This conclusion is based on cumulative geophysical, hydrographic, metallogenical and mineral geochemistry evidences. The study area is located within fertile ground in the border of the São Francisco craton, close to other diamond primary sources and secondary deposits. This kimberlitic target is the only known in the Santo Antônio River basin. In addition, the known mineralized gravels of this river, worked in the past by "garimpeiros", have evidence of a short transport (angular pebbles and blocks), further evidence of a nearby source. The original data collected in the "Minas Gerais Aerogeophysical Survey Program" was processed and analyzed with the Euler Deconvolution method, implemented in software Oasis Montaj. With the exception of the Canastra-3 body anomaly, all others in the study were classified as non-kimberlitic. Recent sampling work on the weathered top of the Canastra-3 Kimberlite recovered indicator minerals, notably a high proportion of pyrope garnets of the G-10 type, which is unusual among the kimberlites of the region.
Related Topics
- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.1590/0370-44672018730051
- https://www.scielo.br/j/remi/a/dc7bTkVnrHYxnWxJzjfWvCL/?format=pdf&lang=en
- OA Status
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- OpenAlex ID
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Raw OpenAlex JSON
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https://openalex.org/W2996481232Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.1590/0370-44672018730051Digital Object Identifier
- Title
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Diamonds from the Santo Antônio River (Delfinópolis, Minas Gerais): probable relationship with the Canastra-3 KimberliteWork title
- Type
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articleOpenAlex work type
- Language
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enPrimary language
- Publication year
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2019Year of publication
- Publication date
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2019-12-20Full publication date if available
- Authors
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Mario Luiz de Sá Carneiro Chaves, João Paulo de Paula Caldas, Kerley Wanderson Andrade, Maria Sílvia Carvalho BarbosaList of authors in order
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https://doi.org/10.1590/0370-44672018730051Publisher landing page
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https://www.scielo.br/j/remi/a/dc7bTkVnrHYxnWxJzjfWvCL/?format=pdf&lang=enDirect link to full text PDF
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goldOpen access status per OpenAlex
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https://www.scielo.br/j/remi/a/dc7bTkVnrHYxnWxJzjfWvCL/?format=pdf&lang=enDirect OA link when available
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Kimberlite, Geology, Geochemistry, Forestry, Geography, Mantle (geology)Top concepts (fields/topics) attached by OpenAlex
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0Total citation count in OpenAlex
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18Number of works referenced by this work
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10Other works algorithmically related by OpenAlex
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| abstract_inverted_index.source. | 112 |
| abstract_inverted_index.sources | 65 |
| abstract_inverted_index.unusual | 182 |
| abstract_inverted_index.(angular | 103 |
| abstract_inverted_index.Abstract | 0 |
| abstract_inverted_index.Antônio | 24, 79 |
| abstract_inverted_index.Gerais). | 30 |
| abstract_inverted_index.Program" | 123 |
| abstract_inverted_index.alluvial | 16 |
| abstract_inverted_index.analyzed | 127 |
| abstract_inverted_index.anomaly, | 145 |
| abstract_inverted_index.blocks), | 106 |
| abstract_inverted_index.diamonds | 17 |
| abstract_inverted_index.evidence | 98, 108 |
| abstract_inverted_index.magnetic | 7 |
| abstract_inverted_index.original | 114 |
| abstract_inverted_index.sampling | 156 |
| abstract_inverted_index.software | 135 |
| abstract_inverted_index.Francisco | 58 |
| abstract_inverted_index.addition, | 83 |
| abstract_inverted_index.collected | 116 |
| abstract_inverted_index.deposits. | 68 |
| abstract_inverted_index.exception | 140 |
| abstract_inverted_index.indicator | 167 |
| abstract_inverted_index.minerals, | 168 |
| abstract_inverted_index.processed | 125 |
| abstract_inverted_index.recovered | 18, 166 |
| abstract_inverted_index.secondary | 67 |
| abstract_inverted_index.transport | 102 |
| abstract_inverted_index.weathered | 160 |
| abstract_inverted_index.Canastra-3 | 5, 143, 164 |
| abstract_inverted_index.Kimberlite | 6, 165 |
| abstract_inverted_index.classified | 152 |
| abstract_inverted_index.conclusion | 32 |
| abstract_inverted_index.cumulative | 36 |
| abstract_inverted_index.evidences. | 43 |
| abstract_inverted_index.identifies | 3 |
| abstract_inverted_index.proportion | 172 |
| abstract_inverted_index.implemented | 133 |
| abstract_inverted_index.kimberlites | 185 |
| abstract_inverted_index.kimberlitic | 70 |
| abstract_inverted_index.mineralized | 86 |
| abstract_inverted_index.geochemistry | 42 |
| abstract_inverted_index.geophysical, | 37 |
| abstract_inverted_index.southwestern | 28 |
| abstract_inverted_index."garimpeiros" | 20 |
| abstract_inverted_index.Deconvolution | 131 |
| abstract_inverted_index.hydrographic, | 38 |
| abstract_inverted_index."garimpeiros", | 96 |
| abstract_inverted_index.metallogenical | 39 |
| abstract_inverted_index.(Delfinópolis, | 27 |
| abstract_inverted_index.Aerogeophysical | 121 |
| abstract_inverted_index.non-kimberlitic. | 154 |
| cited_by_percentile_year | |
| countries_distinct_count | 1 |
| institutions_distinct_count | 4 |
| citation_normalized_percentile.value | 0.13103195 |
| citation_normalized_percentile.is_in_top_1_percent | False |
| citation_normalized_percentile.is_in_top_10_percent | False |