Geology of the Larsemann Hills 2004

The Larsemann Hills region is dominated by two major lithological associations, a Palaeoproterozoic felsic/mafic orthogneiss complex (Søstrene Orthogneiss) which occurs as basement to a sequence of pelitic, psammitic and felsic paragneiss (supergroup = Brattstrand Paragneiss) and felsic intrusives....

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Bibliographic Details
Other Authors: Australian Antarctic Division (isOwnedBy)
Format: Dataset
Language:unknown
Published: data.gov.au
Subjects:
AMD
GIS
Map
Online Access:https://researchdata.edu.au/geology-larsemann-hills-2004/1434810
http://data.gov.au/dataset/1f1551b9-6fc9-43b5-951a-6b378e31f2ad
id ftands:oai:ands.org.au::1434810
record_format openpolar
spelling ftands:oai:ands.org.au::1434810 2023-09-05T13:12:58+02:00 Geology of the Larsemann Hills 2004 Australian Antarctic Division (isOwnedBy) Spatial: 75.95,-69.48 76.55,-69.48 76.55,-69.33 75.95,-69.33 75.95,-69.48 https://researchdata.edu.au/geology-larsemann-hills-2004/1434810 http://data.gov.au/dataset/1f1551b9-6fc9-43b5-951a-6b378e31f2ad unknown data.gov.au https://researchdata.edu.au/geology-larsemann-hills-2004/1434810 http://data.gov.au/dataset/1f1551b9-6fc9-43b5-951a-6b378e31f2ad aad-lars-geology-2004 Australian Antarctic Division AERIAL PHOTOGRAPHS AMD AMD-AU CEOS CONTINENT - ANTARCTICA - Larsemann Hills EARTH SCIENCE - SOLID EARTH - GEOMORPHIC LANDFORMS-PROCESSES - TECTONIC LANDFORMS EARTH SCIENCE - SOLID EARTH - ROCKS-MINERALS-CRYSTALS EARTH SCIENCE - SOLID EARTH - ROCKS-MINERALS-CRYSTALS - METAMORPHIC ROCKS GEOGRAPHIC REGION - POLAR GIS Geology Larsemann Hills Map dataset ftands 2023-08-14T22:32:41Z The Larsemann Hills region is dominated by two major lithological associations, a Palaeoproterozoic felsic/mafic orthogneiss complex (Søstrene 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 Søstrene 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 Søstrene 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.\r\n\r\nSee the document available for download at the URL given below for further information. Point of truth URL of this metadata record - Point of truth URL of this metadata record Download point for the data - shapefiles - Download point for the data - shapefiles Download point for the data - map produced from the data - Download point for the data - map produced from the data Public information for ASAC project 2350 - Public information for ASAC project 2350 Citation reference for this metadata record and dataset - Citation reference for this metadata record and dataset Dataset Antarc* Antarctica Research Data Australia (Australian National Data Service - ANDS) Larsemann Hills ENVELOPE(76.217,76.217,-69.400,-69.400) Søstrene ENVELOPE(75.503,75.503,-69.588,-69.588)
institution Open Polar
collection Research Data Australia (Australian National Data Service - ANDS)
op_collection_id ftands
language unknown
topic AERIAL PHOTOGRAPHS
AMD
AMD-AU
CEOS
CONTINENT - ANTARCTICA - Larsemann Hills
EARTH SCIENCE - SOLID EARTH - GEOMORPHIC LANDFORMS-PROCESSES - TECTONIC LANDFORMS
EARTH SCIENCE - SOLID EARTH - ROCKS-MINERALS-CRYSTALS
EARTH SCIENCE - SOLID EARTH - ROCKS-MINERALS-CRYSTALS - METAMORPHIC ROCKS
GEOGRAPHIC REGION - POLAR
GIS
Geology
Larsemann Hills
Map
spellingShingle AERIAL PHOTOGRAPHS
AMD
AMD-AU
CEOS
CONTINENT - ANTARCTICA - Larsemann Hills
EARTH SCIENCE - SOLID EARTH - GEOMORPHIC LANDFORMS-PROCESSES - TECTONIC LANDFORMS
EARTH SCIENCE - SOLID EARTH - ROCKS-MINERALS-CRYSTALS
EARTH SCIENCE - SOLID EARTH - ROCKS-MINERALS-CRYSTALS - METAMORPHIC ROCKS
GEOGRAPHIC REGION - POLAR
GIS
Geology
Larsemann Hills
Map
Geology of the Larsemann Hills 2004
topic_facet AERIAL PHOTOGRAPHS
AMD
AMD-AU
CEOS
CONTINENT - ANTARCTICA - Larsemann Hills
EARTH SCIENCE - SOLID EARTH - GEOMORPHIC LANDFORMS-PROCESSES - TECTONIC LANDFORMS
EARTH SCIENCE - SOLID EARTH - ROCKS-MINERALS-CRYSTALS
EARTH SCIENCE - SOLID EARTH - ROCKS-MINERALS-CRYSTALS - METAMORPHIC ROCKS
GEOGRAPHIC REGION - POLAR
GIS
Geology
Larsemann Hills
Map
description The Larsemann Hills region is dominated by two major lithological associations, a Palaeoproterozoic felsic/mafic orthogneiss complex (Søstrene 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 Søstrene 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 Søstrene 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.\r\n\r\nSee the document available for download at the URL given below for further information. Point of truth URL of this metadata record - Point of truth URL of this metadata record Download point for the data - shapefiles - Download point for the data - shapefiles Download point for the data - map produced from the data - Download point for the data - map produced from the data Public information for ASAC project 2350 - Public information for ASAC project 2350 Citation reference for this metadata record and dataset - Citation reference for this metadata record and dataset
author2 Australian Antarctic Division (isOwnedBy)
format Dataset
title Geology of the Larsemann Hills 2004
title_short Geology of the Larsemann Hills 2004
title_full Geology of the Larsemann Hills 2004
title_fullStr Geology of the Larsemann Hills 2004
title_full_unstemmed Geology of the Larsemann Hills 2004
title_sort geology of the larsemann hills 2004
publisher data.gov.au
url https://researchdata.edu.au/geology-larsemann-hills-2004/1434810
http://data.gov.au/dataset/1f1551b9-6fc9-43b5-951a-6b378e31f2ad
op_coverage Spatial: 75.95,-69.48 76.55,-69.48 76.55,-69.33 75.95,-69.33 75.95,-69.48
long_lat ENVELOPE(76.217,76.217,-69.400,-69.400)
ENVELOPE(75.503,75.503,-69.588,-69.588)
geographic Larsemann Hills
Søstrene
geographic_facet Larsemann Hills
Søstrene
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Australian Antarctic Division
op_relation https://researchdata.edu.au/geology-larsemann-hills-2004/1434810
http://data.gov.au/dataset/1f1551b9-6fc9-43b5-951a-6b378e31f2ad
aad-lars-geology-2004
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