Geology Map of the Larsemann Hills 2004
The Larsemann Hills region is dominated by two major lithological associations, a Palaeoproterozoic felsic/mafic orthogneiss complex (Sostrene Orthogneiss) which occurs as basement to a sequence of pelitic, psammitic and felsic paragneiss (supergroup = Brattstrand Paragneiss) and felsic intrusives....
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Australian Antarctic Data Centre
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Online Access: | https://researchdata.ands.org.au/geology-map-larsemann-hills-2004/701238 https://doi.org/10.26179/5beba1b8ddecd https://data.aad.gov.au/metadata/records/lars_geology_2004 http://nla.gov.au/nla.party-617536 |
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ftands:oai:ands.org.au::701238 2023-05-15T13:46:59+02:00 Geology Map of the Larsemann Hills 2004 CARSON, CHRISTOPHER (hasPrincipalInvestigator) CARSON, CHRISTOPHER (processor) GREW, EDWARD (hasPrincipalInvestigator) Australian Antarctic Data Centre (publisher) Spatial: northlimit=-69.33; southlimit=-69.48; westlimit=75.95; eastLimit=76.55; projection=WGS84 Temporal: From 2003-11-16 to 2004-02-04 https://researchdata.ands.org.au/geology-map-larsemann-hills-2004/701238 https://doi.org/10.26179/5beba1b8ddecd https://data.aad.gov.au/metadata/records/lars_geology_2004 http://nla.gov.au/nla.party-617536 unknown Australian Antarctic Data Centre https://researchdata.ands.org.au/geology-map-larsemann-hills-2004/701238 3fcddd06-14e1-4305-9698-6d2eac299b73 doi:10.26179/5beba1b8ddecd lars_geology_2004 https://data.aad.gov.au/metadata/records/lars_geology_2004 http://nla.gov.au/nla.party-617536 Australian Antarctic Data Centre geoscientificInformation TECTONIC LANDFORMS EARTH SCIENCE SOLID EARTH GEOMORPHIC LANDFORMS/PROCESSES METAMORPHIC ROCKS ROCKS/MINERALS/CRYSTALS Larsemann Hills Geology GIS Map VISUAL OBSERVATIONS AERIAL PHOTOGRAPHS CONTINENT > ANTARCTICA > GEOGRAPHIC REGION > POLAR dataset ftands https://doi.org/10.26179/5beba1b8ddecd 2020-01-05T21:18:38Z The Larsemann Hills region is dominated by two major lithological associations, a Palaeoproterozoic felsic/mafic orthogneiss complex (Sostrene Orthogneiss) which occurs as basement to a sequence of pelitic, psammitic and felsic paragneiss (supergroup = Brattstrand Paragneiss) and felsic intrusives. The depositional age of the Brattstrand Paragneiss sequences are controversial but isotopic data suggest derivation from the basement Sostrene Orthogneiss. Current geochronology indicates that the region experienced medium to low pressure granulite-facies metamorphism during the Early Palaeozoic (~500 Ma). Although the paragneiss sequences record no evidence of earlier metamorphism, relicts of a previous metamorphic event at ~1000 Ma are preserved in the Sostrene Orthogneiss. Within the Larsemann Hills region, the Early Palaeozoic event is characterised by peak metamorphism of ~7 kbar at ~800-850 degrees C, with the post-peak evolution characterised by decompression, with some cooling, to 4 kbars at 750 degrees C, then to 2-3 kbar at 600-650 degrees C during final stages of orogenesis, with exhumation largely driven by crustal extension. Tectonic models generally argue for a continental-continental collisional scenario, with thermal input derived from a thinned mantle lithosphere. See the document available for download at the provided URL for further information. Dataset Antarc* Antarctica Research Data Australia (Australian National Data Service - ANDS) Larsemann Hills ENVELOPE(76.217,76.217,-69.400,-69.400) Sostrene ENVELOPE(75.503,75.503,-69.588,-69.588) ENVELOPE(75.95,76.55,-69.33,-69.48) |
institution |
Open Polar |
collection |
Research Data Australia (Australian National Data Service - ANDS) |
op_collection_id |
ftands |
language |
unknown |
topic |
geoscientificInformation TECTONIC LANDFORMS EARTH SCIENCE SOLID EARTH GEOMORPHIC LANDFORMS/PROCESSES METAMORPHIC ROCKS ROCKS/MINERALS/CRYSTALS Larsemann Hills Geology GIS Map VISUAL OBSERVATIONS AERIAL PHOTOGRAPHS CONTINENT > ANTARCTICA > GEOGRAPHIC REGION > POLAR |
spellingShingle |
geoscientificInformation TECTONIC LANDFORMS EARTH SCIENCE SOLID EARTH GEOMORPHIC LANDFORMS/PROCESSES METAMORPHIC ROCKS ROCKS/MINERALS/CRYSTALS Larsemann Hills Geology GIS Map VISUAL OBSERVATIONS AERIAL PHOTOGRAPHS CONTINENT > ANTARCTICA > GEOGRAPHIC REGION > POLAR Geology Map of the Larsemann Hills 2004 |
topic_facet |
geoscientificInformation TECTONIC LANDFORMS EARTH SCIENCE SOLID EARTH GEOMORPHIC LANDFORMS/PROCESSES METAMORPHIC ROCKS ROCKS/MINERALS/CRYSTALS Larsemann Hills Geology GIS Map VISUAL OBSERVATIONS AERIAL PHOTOGRAPHS CONTINENT > ANTARCTICA > GEOGRAPHIC REGION > POLAR |
description |
The Larsemann Hills region is dominated by two major lithological associations, a Palaeoproterozoic felsic/mafic orthogneiss complex (Sostrene Orthogneiss) which occurs as basement to a sequence of pelitic, psammitic and felsic paragneiss (supergroup = Brattstrand Paragneiss) and felsic intrusives. The depositional age of the Brattstrand Paragneiss sequences are controversial but isotopic data suggest derivation from the basement Sostrene Orthogneiss. Current geochronology indicates that the region experienced medium to low pressure granulite-facies metamorphism during the Early Palaeozoic (~500 Ma). Although the paragneiss sequences record no evidence of earlier metamorphism, relicts of a previous metamorphic event at ~1000 Ma are preserved in the Sostrene Orthogneiss. Within the Larsemann Hills region, the Early Palaeozoic event is characterised by peak metamorphism of ~7 kbar at ~800-850 degrees C, with the post-peak evolution characterised by decompression, with some cooling, to 4 kbars at 750 degrees C, then to 2-3 kbar at 600-650 degrees C during final stages of orogenesis, with exhumation largely driven by crustal extension. Tectonic models generally argue for a continental-continental collisional scenario, with thermal input derived from a thinned mantle lithosphere. See the document available for download at the provided URL for further information. |
author2 |
CARSON, CHRISTOPHER (hasPrincipalInvestigator) CARSON, CHRISTOPHER (processor) GREW, EDWARD (hasPrincipalInvestigator) Australian Antarctic Data Centre (publisher) |
format |
Dataset |
title |
Geology Map of the Larsemann Hills 2004 |
title_short |
Geology Map of the Larsemann Hills 2004 |
title_full |
Geology Map of the Larsemann Hills 2004 |
title_fullStr |
Geology Map of the Larsemann Hills 2004 |
title_full_unstemmed |
Geology Map of the Larsemann Hills 2004 |
title_sort |
geology map of the larsemann hills 2004 |
publisher |
Australian Antarctic Data Centre |
url |
https://researchdata.ands.org.au/geology-map-larsemann-hills-2004/701238 https://doi.org/10.26179/5beba1b8ddecd https://data.aad.gov.au/metadata/records/lars_geology_2004 http://nla.gov.au/nla.party-617536 |
op_coverage |
Spatial: northlimit=-69.33; southlimit=-69.48; westlimit=75.95; eastLimit=76.55; projection=WGS84 Temporal: From 2003-11-16 to 2004-02-04 |
long_lat |
ENVELOPE(76.217,76.217,-69.400,-69.400) ENVELOPE(75.503,75.503,-69.588,-69.588) ENVELOPE(75.95,76.55,-69.33,-69.48) |
geographic |
Larsemann Hills Sostrene |
geographic_facet |
Larsemann Hills Sostrene |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
Australian Antarctic Data Centre |
op_relation |
https://researchdata.ands.org.au/geology-map-larsemann-hills-2004/701238 3fcddd06-14e1-4305-9698-6d2eac299b73 doi:10.26179/5beba1b8ddecd lars_geology_2004 https://data.aad.gov.au/metadata/records/lars_geology_2004 http://nla.gov.au/nla.party-617536 |
op_doi |
https://doi.org/10.26179/5beba1b8ddecd |
_version_ |
1766246036663173120 |