Zeolite zones in East Greenland: use of native copper by pre‐contact Inuit?
Zeolites are a diverse group of calcium and sodium aluminosilicate minerals. They are tectosilicates (3‐D arrays of SiO 4 tetrahedra), but vary in chemistry and crystal symmetry. Some readily exchange sodium for calcium and are used as water softeners. They also find applications as molecular sieves...
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crwiley:10.1111/gto.12230 2024-06-02T08:02:01+00:00 Zeolite zones in East Greenland: use of native copper by pre‐contact Inuit? Brooks, Kent 2018 http://dx.doi.org/10.1111/gto.12230 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fgto.12230 https://onlinelibrary.wiley.com/doi/pdf/10.1111/gto.12230 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Geology Today volume 34, issue 3, page 109-112 ISSN 0266-6979 1365-2451 journal-article 2018 crwiley https://doi.org/10.1111/gto.12230 2024-05-03T11:23:57Z Zeolites are a diverse group of calcium and sodium aluminosilicate minerals. They are tectosilicates (3‐D arrays of SiO 4 tetrahedra), but vary in chemistry and crystal symmetry. Some readily exchange sodium for calcium and are used as water softeners. They also find applications as molecular sieves in petroleum refining, although the bulk of zeolites used industrially today are synthetic. These minerals form at low temperatures under well‐defined conditions and can be used as indicators of palaeotemperatures. In the same environment, but at higher temperatures, other minerals form including quartz, calcite, prehnite and even native copper. The Inuit of East Greenland, a Stone Age people, may have utilized native copper from this environment as did the Copper Inuit of the central Canadian Arctic. Article in Journal/Newspaper Arctic East Greenland Greenland inuit Wiley Online Library Arctic Greenland Geology Today 34 3 109 112 |
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Wiley Online Library |
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English |
description |
Zeolites are a diverse group of calcium and sodium aluminosilicate minerals. They are tectosilicates (3‐D arrays of SiO 4 tetrahedra), but vary in chemistry and crystal symmetry. Some readily exchange sodium for calcium and are used as water softeners. They also find applications as molecular sieves in petroleum refining, although the bulk of zeolites used industrially today are synthetic. These minerals form at low temperatures under well‐defined conditions and can be used as indicators of palaeotemperatures. In the same environment, but at higher temperatures, other minerals form including quartz, calcite, prehnite and even native copper. The Inuit of East Greenland, a Stone Age people, may have utilized native copper from this environment as did the Copper Inuit of the central Canadian Arctic. |
format |
Article in Journal/Newspaper |
author |
Brooks, Kent |
spellingShingle |
Brooks, Kent Zeolite zones in East Greenland: use of native copper by pre‐contact Inuit? |
author_facet |
Brooks, Kent |
author_sort |
Brooks, Kent |
title |
Zeolite zones in East Greenland: use of native copper by pre‐contact Inuit? |
title_short |
Zeolite zones in East Greenland: use of native copper by pre‐contact Inuit? |
title_full |
Zeolite zones in East Greenland: use of native copper by pre‐contact Inuit? |
title_fullStr |
Zeolite zones in East Greenland: use of native copper by pre‐contact Inuit? |
title_full_unstemmed |
Zeolite zones in East Greenland: use of native copper by pre‐contact Inuit? |
title_sort |
zeolite zones in east greenland: use of native copper by pre‐contact inuit? |
publisher |
Wiley |
publishDate |
2018 |
url |
http://dx.doi.org/10.1111/gto.12230 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fgto.12230 https://onlinelibrary.wiley.com/doi/pdf/10.1111/gto.12230 |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
Arctic East Greenland Greenland inuit |
genre_facet |
Arctic East Greenland Greenland inuit |
op_source |
Geology Today volume 34, issue 3, page 109-112 ISSN 0266-6979 1365-2451 |
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http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/gto.12230 |
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Geology Today |
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34 |
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3 |
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109 |
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112 |
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1800746519741071360 |