Acid sulphate alteration hydrothermal environment
Volcanic-hosted advanced argillie alteration on Barton Peninsula comprises an assemblage of chalcedonic silica, alunite family minerals, pyrophyllite, pyrite, native sulphur, zunyite and rutile, characteristic of an acid sulphate-type pithermal system. The minerals minamiite, (Na0.36Cao.27K0.1[]0.27...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.604.4449 2023-05-15T14:02:37+02:00 Acid sulphate alteration hydrothermal environment King George Island Debbie C. Armstrong The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.604.4449 http://www.minersoc.org/pages/Archive-MM/Volume_59/59-396-429.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.604.4449 http://www.minersoc.org/pages/Archive-MM/Volume_59/59-396-429.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.minersoc.org/pages/Archive-MM/Volume_59/59-396-429.pdf volcanic-hosted argillic alteration acid sulphate-type epithermal system Antarctica text ftciteseerx 2016-01-08T14:11:12Z Volcanic-hosted advanced argillie alteration on Barton Peninsula comprises an assemblage of chalcedonic silica, alunite family minerals, pyrophyllite, pyrite, native sulphur, zunyite and rutile, characteristic of an acid sulphate-type pithermal system. The minerals minamiite, (Na0.36Cao.27K0.1[]0.27)A13(SO4)2(OH)6, and zunyite, Al13SisO2o(OH,F)IsC1, are reported at this locality, and in Antarctica, for the first time. The WNW-striking, 1 km-long zone of alteration is hosted by early Tertiary andesitic rocks and contained in a 1.5 kin-wide depression, rimmed by an arcuate ridge, probably representing a volcanic crater or small caldera structure. Stability relations of minerals in the advanced argillic alteration zone indicate alteration took place under acidic conditions in the near-surface environment. Mineralogical and textural evidence also suggest alteration occurred in a magmatic hydrothermal system, possibly with a magmatic steam component, rather than in a supergene or steam-heated nvironment. Text Antarc* Antarctica Unknown Barton ENVELOPE(-58.733,-58.733,-62.233,-62.233) Barton Peninsula ENVELOPE(-58.741,-58.741,-62.227,-62.227) |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
topic |
volcanic-hosted argillic alteration acid sulphate-type epithermal system Antarctica |
spellingShingle |
volcanic-hosted argillic alteration acid sulphate-type epithermal system Antarctica King George Island Debbie C. Armstrong Acid sulphate alteration hydrothermal environment |
topic_facet |
volcanic-hosted argillic alteration acid sulphate-type epithermal system Antarctica |
description |
Volcanic-hosted advanced argillie alteration on Barton Peninsula comprises an assemblage of chalcedonic silica, alunite family minerals, pyrophyllite, pyrite, native sulphur, zunyite and rutile, characteristic of an acid sulphate-type pithermal system. The minerals minamiite, (Na0.36Cao.27K0.1[]0.27)A13(SO4)2(OH)6, and zunyite, Al13SisO2o(OH,F)IsC1, are reported at this locality, and in Antarctica, for the first time. The WNW-striking, 1 km-long zone of alteration is hosted by early Tertiary andesitic rocks and contained in a 1.5 kin-wide depression, rimmed by an arcuate ridge, probably representing a volcanic crater or small caldera structure. Stability relations of minerals in the advanced argillic alteration zone indicate alteration took place under acidic conditions in the near-surface environment. Mineralogical and textural evidence also suggest alteration occurred in a magmatic hydrothermal system, possibly with a magmatic steam component, rather than in a supergene or steam-heated nvironment. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
King George Island Debbie C. Armstrong |
author_facet |
King George Island Debbie C. Armstrong |
author_sort |
King George Island |
title |
Acid sulphate alteration hydrothermal environment |
title_short |
Acid sulphate alteration hydrothermal environment |
title_full |
Acid sulphate alteration hydrothermal environment |
title_fullStr |
Acid sulphate alteration hydrothermal environment |
title_full_unstemmed |
Acid sulphate alteration hydrothermal environment |
title_sort |
acid sulphate alteration hydrothermal environment |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.604.4449 http://www.minersoc.org/pages/Archive-MM/Volume_59/59-396-429.pdf |
long_lat |
ENVELOPE(-58.733,-58.733,-62.233,-62.233) ENVELOPE(-58.741,-58.741,-62.227,-62.227) |
geographic |
Barton Barton Peninsula |
geographic_facet |
Barton Barton Peninsula |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
http://www.minersoc.org/pages/Archive-MM/Volume_59/59-396-429.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.604.4449 http://www.minersoc.org/pages/Archive-MM/Volume_59/59-396-429.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766272930212216832 |