Geology of the Stillwell Hills
The Stillwell Hills region comprises granulite facies gneisses which record evidence for multiple periods of deformation and metamorphism spanning more than 2500 Million years. The predominant orthogneiss package (Stillwell Orthogneiss) represents the margin of an Archaean craton exposed in Enderby...
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Online Access: | https://researchdata.edu.au/geology-stillwell-hills/1936329 http://data.gov.au/dataset/d1bf9f10-3b92-4f2d-9519-880dd7c772fa |
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ftands:oai:ands.org.au::1936329 2023-09-05T13:13:27+02:00 Geology of the Stillwell Hills Geoscience Australia (isOwnedBy) Spatial: 59.0,-68.0 60.0,-68.0 60.0,-67.0 59.0,-67.0 59.0,-68.0 Spatial: true https://researchdata.edu.au/geology-stillwell-hills/1936329 http://data.gov.au/dataset/d1bf9f10-3b92-4f2d-9519-880dd7c772fa unknown data.gov.au https://researchdata.edu.au/geology-stillwell-hills/1936329 http://data.gov.au/dataset/d1bf9f10-3b92-4f2d-9519-880dd7c772fa geology-of-the-stillwell-hills Geoscience Australia 25K scale Antarctic data Geological Map Geology marine dataset ftands 2023-08-14T23:02:20Z The Stillwell Hills region comprises granulite facies gneisses which record evidence for multiple periods of deformation and metamorphism spanning more than 2500 Million years. The predominant orthogneiss package (Stillwell Orthogneiss) represents the margin of an Archaean craton exposed in Enderby Land, some 150 km to the west that was reworked during the late Proterozoic. Younger additions to the crust include Palaeoproterozoic charnockitic gneiss (Scoresby Charnockite) and Meso-Neoproterozoic mafic sills and dykes (Point Noble Gneiss, Kemp Dykes) and felsic pegmatites (Cosgrove Pegmatites). Subordinate supracrustal rocks, including metaquartzite, metapelitic, metapsammitic and calc-silicate gneiss (Dovers Paragneiss, Sperring Paragneiss, Stefansson Paragneiss, Keel Layered Paragneiss, Ives Gneiss) are intercalated and interfolded with the Archaean-Palaeoproterozoic orthogneisses.\n\nYou can also purchase hard copies of Geoscience Australia data and other products at http://www.ga.gov.au/products-services/how-to-order-products/sales-centre.html Download the file (pdf) - Download the file (pdf) Dataset Antarc* Antarctic Enderby Land Research Data Australia (Australian National Data Service - ANDS) Antarctic Dovers ENVELOPE(97.167,97.167,-66.483,-66.483) Point Noble ENVELOPE(59.473,59.473,-67.342,-67.342) Scoresby ENVELOPE(162.750,162.750,-66.567,-66.567) Stefansson ENVELOPE(-62.417,-62.417,-69.467,-69.467) Stillwell Hills ENVELOPE(59.467,59.467,-67.417,-67.417) |
institution |
Open Polar |
collection |
Research Data Australia (Australian National Data Service - ANDS) |
op_collection_id |
ftands |
language |
unknown |
topic |
25K scale Antarctic data Geological Map Geology marine |
spellingShingle |
25K scale Antarctic data Geological Map Geology marine Geology of the Stillwell Hills |
topic_facet |
25K scale Antarctic data Geological Map Geology marine |
description |
The Stillwell Hills region comprises granulite facies gneisses which record evidence for multiple periods of deformation and metamorphism spanning more than 2500 Million years. The predominant orthogneiss package (Stillwell Orthogneiss) represents the margin of an Archaean craton exposed in Enderby Land, some 150 km to the west that was reworked during the late Proterozoic. Younger additions to the crust include Palaeoproterozoic charnockitic gneiss (Scoresby Charnockite) and Meso-Neoproterozoic mafic sills and dykes (Point Noble Gneiss, Kemp Dykes) and felsic pegmatites (Cosgrove Pegmatites). Subordinate supracrustal rocks, including metaquartzite, metapelitic, metapsammitic and calc-silicate gneiss (Dovers Paragneiss, Sperring Paragneiss, Stefansson Paragneiss, Keel Layered Paragneiss, Ives Gneiss) are intercalated and interfolded with the Archaean-Palaeoproterozoic orthogneisses.\n\nYou can also purchase hard copies of Geoscience Australia data and other products at http://www.ga.gov.au/products-services/how-to-order-products/sales-centre.html Download the file (pdf) - Download the file (pdf) |
author2 |
Geoscience Australia (isOwnedBy) |
format |
Dataset |
title |
Geology of the Stillwell Hills |
title_short |
Geology of the Stillwell Hills |
title_full |
Geology of the Stillwell Hills |
title_fullStr |
Geology of the Stillwell Hills |
title_full_unstemmed |
Geology of the Stillwell Hills |
title_sort |
geology of the stillwell hills |
publisher |
data.gov.au |
url |
https://researchdata.edu.au/geology-stillwell-hills/1936329 http://data.gov.au/dataset/d1bf9f10-3b92-4f2d-9519-880dd7c772fa |
op_coverage |
Spatial: 59.0,-68.0 60.0,-68.0 60.0,-67.0 59.0,-67.0 59.0,-68.0 Spatial: true |
long_lat |
ENVELOPE(97.167,97.167,-66.483,-66.483) ENVELOPE(59.473,59.473,-67.342,-67.342) ENVELOPE(162.750,162.750,-66.567,-66.567) ENVELOPE(-62.417,-62.417,-69.467,-69.467) ENVELOPE(59.467,59.467,-67.417,-67.417) |
geographic |
Antarctic Dovers Point Noble Scoresby Stefansson Stillwell Hills |
geographic_facet |
Antarctic Dovers Point Noble Scoresby Stefansson Stillwell Hills |
genre |
Antarc* Antarctic Enderby Land |
genre_facet |
Antarc* Antarctic Enderby Land |
op_source |
Geoscience Australia |
op_relation |
https://researchdata.edu.au/geology-stillwell-hills/1936329 http://data.gov.au/dataset/d1bf9f10-3b92-4f2d-9519-880dd7c772fa geology-of-the-stillwell-hills |
_version_ |
1776204724526120960 |