Data

Geology of the Stillwell Hills GIS Dataset

Australian Antarctic Division
Carson, C., Woods, M. and Halpin, J. ; CARSON, CHRISTOPHER ; HALPIN, JACQUELINE ; WOODS, MURRAY
Viewed: [[ro.stat.viewed]] Cited: [[ro.stat.cited]] Accessed: [[ro.stat.accessed]]
ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=http://data.aad.gov.au/metadata/stillwell_geology_gis&rft.title=Geology of the Stillwell Hills GIS Dataset&rft.identifier=http://data.aad.gov.au/metadata/stillwell_geology_gis&rft.publisher=Australian Antarctic Data Centre&rft.description=The Stillwell Hills region comprises granulite-facies gneisses which record evidence for multiple episodes of deformation and metamorphism spanning more than 2500 million years. The predominant orthogneiss package (Stillwell Orthogneiss) is thought to represent 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 Paragneiss, Ives Paragneiss) are intercalated and infolded with the Archaean-Palaeoproterozoic orthogneisses. This Dataset is derived from the map product 'The Geology of the Stillwell Hills, Antarctica'.This metadata record was created using information in Geoscience Australia's metadata record at http://www.ga.gov.au/metadata-gateway/metadata/record/78535/Progress Code: completed&rft.creator=Carson, C., Woods, M. and Halpin, J. &rft.creator=CARSON, CHRISTOPHER &rft.creator=HALPIN, JACQUELINE &rft.creator=WOODS, MURRAY &rft.date=2016&rft.coverage=westlimit=59.3618; southlimit=-67.4645; eastlimit=59.5698; northlimit=-67.2942&rft.coverage=westlimit=59.3618; southlimit=-67.4645; eastlimit=59.5698; northlimit=-67.2942&rft_rights=The data and metadata are available for download from the Geoscience Australia website (see a Related URL).&rft_rights=Attribution 4.0 International (CC BY 4.0) https://creativecommons.org/licenses/by/4.0/legalcode&rft_rights=This data set conforms to the CCBY Attribution License (http://creativecommons.org/licenses/by/4.0/). Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=stillwell_geology_gis when using these data.&rft_rights=This metadata record is publicly available.&rft_subject=geoscientificInformation&rft_subject=EARTH SCIENCE > SOLID EARTH > ROCKS/MINERALS/CRYSTALS > METAMORPHIC ROCKS&rft_subject=EARTH SCIENCE > SOLID EARTH > ROCKS/MINERALS/CRYSTALS > METAMORPHIC ROCKS > METAMORPHIC ROCK FORMATION&rft_subject=AMD/AU&rft_subject=AMD&rft_subject=CEOS&rft_subject=GEOGRAPHIC REGION > POLAR&rft_subject=CONTINENT > ANTARCTICA&rft.type=dataset&rft.language=English Access the data

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Open Licence view details
CC-BY

Attribution 4.0 International (CC BY 4.0)
https://creativecommons.org/licenses/by/4.0/legalcode

The data and metadata are available for download from the Geoscience Australia website (see a Related URL).

This data set conforms to the CCBY Attribution License (http://creativecommons.org/licenses/by/4.0/).

Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=stillwell_geology_gis when using these data.

This metadata record is publicly available.

Access:

Other

Full description

The Stillwell Hills region comprises granulite-facies gneisses which record evidence for multiple episodes of deformation and metamorphism spanning more than 2500 million years. The predominant orthogneiss package (Stillwell Orthogneiss) is thought to represent 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 Paragneiss, Ives Paragneiss) are intercalated and infolded with the Archaean-Palaeoproterozoic orthogneisses.
This Dataset is derived from the map product 'The Geology of the Stillwell Hills, Antarctica'.

This metadata record was created using information in Geoscience Australia's metadata record at
http://www.ga.gov.au/metadata-gateway/metadata/record/78535/

Lineage

Progress Code: completed

Data time period: 1996-09-30 to 2016-07-28

This dataset is part of a larger collection

Click to explore relationships graph

59.5698,-67.2942 59.5698,-67.4645 59.3618,-67.4645 59.3618,-67.2942 59.5698,-67.2942

59.4658,-67.37935

text: westlimit=59.3618; southlimit=-67.4645; eastlimit=59.5698; northlimit=-67.2942

Other Information
Metadata record about geological mapping of the Stillwell Hills (EXTENDED METADATA)

uri : http://data.aad.gov.au/metadata/records/ASAC_1150

See the original Geoscience Australia metadata record and access the data (GET DATA)

uri : http://www.ga.gov.au/metadata-gateway/metadata/record/78535/

Citation reference for this metadata record and dataset. (VIEW RELATED INFORMATION)

uri : https://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=stillwell_geology_gis

Geology of the Stillwell Hills map (VIEW RELATED INFORMATION)

uri : http://data.aad.gov.au/aadc/mapcat/display_map.cfm?map_id=13521

Identifiers
  • global : stillwell_geology_gis