Data

Geology of the Stillwell Hills

Australian Ocean Data Network
Halpin, J.A ; Clarke, G.L. ; Gerakiteys, C.L. ; Kelly, N.M. ; Fitzherbert, J.A. ; Schroter, F.C. ; Carson, C.
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=https://pid.geoscience.gov.au/dataset/ga/72717&rft.title=Geology of the Stillwell Hills&rft.identifier=https://pid.geoscience.gov.au/dataset/ga/72717&rft.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.Maintenance and Update Frequency: unknownStatement: Unknown&rft.creator=Halpin, J.A &rft.creator=Clarke, G.L. &rft.creator=Gerakiteys, C.L. &rft.creator=Kelly, N.M. &rft.creator=Fitzherbert, J.A. &rft.creator=Schroter, F.C. &rft.creator=Carson, C. &rft.date=2011&rft.coverage=westlimit=59; southlimit=-68; eastlimit=60; northlimit=-67&rft.coverage=westlimit=59; southlimit=-68; eastlimit=60; northlimit=-67&rft_rights=&rft_rights=Creative Commons Attribution 4.0 International Licence&rft_rights=CC-BY&rft_rights=4.0&rft_rights=http://creativecommons.org/licenses/&rft_rights=WWW:LINK-1.0-http--link&rft_rights=Australian Government Security ClassificationSystem&rft_rights=https://www.protectivesecurity.gov.au/Pages/default.aspx&rft_rights=WWW:LINK-1.0-http--link&rft_rights=Creative Commons Attribution 4.0 International Licence http://creativecommons.org/licenses/by/4.0&rft_subject=geoscientificInformation&rft_subject=Geological Map&rft_subject=25K scale&rft_subject=Antarctic data&rft_subject=geology&rft_subject=marine&rft_subject=AQ&rft_subject=GEOLOGY&rft_subject=EARTH SCIENCES&rft_subject=Published_External&rft.type=dataset&rft.language=English Access the data

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CC-BY

Creative Commons Attribution 4.0 International Licence
http://creativecommons.org/licenses/by/4.0

Creative Commons Attribution 4.0 International Licence

CC-BY

4.0

http://creativecommons.org/licenses/

WWW:LINK-1.0-http--link

Australian Government Security ClassificationSystem

https://www.protectivesecurity.gov.au/Pages/default.aspx

WWW:LINK-1.0-http--link

Access:

Open

Contact Information

clientservices@ga.gov.au

Brief 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.

Lineage

Maintenance and Update Frequency: unknown
Statement: Unknown

Issued: 2011

This dataset is part of a larger collection

Click to explore relationships graph

60,-67 60,-68 59,-68 59,-67 60,-67

59.5,-67.5

text: westlimit=59; southlimit=-68; eastlimit=60; northlimit=-67

Subjects

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Other Information
Related product: Geology of the Stillwell Hills GIS dataset

uri : https://pid.geoscience.gov.au/dataset/ga/78535

Download the file (pdf)

uri : https://d28rz98at9flks.cloudfront.net/72717/72717.pdf

Identifiers