Antarctic seismicity and neotectonics

A map of Antarctic intraplate earthquakes, 1900-99, is presented including records from the Global Seismic Network and recordings made at Antarctic seismic observatories and temporary stations. The results show a low but significant level of seismicity through the Transantarctic Mountains and across...

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Bibliographic Details
Main Author: Reading, AM
Other Authors: Gamble, J.A., Skinner, D.N.B., Henrys, S.
Format: Book Part
Language:English
Published: The Royal Society of New Zealand 2002
Subjects:
Online Access:https://eprints.utas.edu.au/1875/
https://eprints.utas.edu.au/1875/1/Reading_2002_Antarctic_Seismicity_%26_Neotectonics.pdf
http://www.rsnz.org/publish/other/antarctica.php
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spelling ftunivtasmania:oai:eprints.utas.edu.au:1875 2023-05-15T13:04:15+02:00 Antarctic seismicity and neotectonics Reading, AM Gamble, J.A. Skinner, D.N.B. Henrys, S. 2002 application/pdf https://eprints.utas.edu.au/1875/ https://eprints.utas.edu.au/1875/1/Reading_2002_Antarctic_Seismicity_%26_Neotectonics.pdf http://www.rsnz.org/publish/other/antarctica.php en eng The Royal Society of New Zealand https://eprints.utas.edu.au/1875/1/Reading_2002_Antarctic_Seismicity_%26_Neotectonics.pdf Reading, AM orcid:0000-0002-9316-7605 2002 , 'Antarctic seismicity and neotectonics', in J.A. Gamble and D.N.B. Skinner and S. Henrys (eds.), Antarctica at the close of a millennium , Royal Society of New Zealand Bulletin, vol. 35 , The Royal Society of New Zealand, Wellington, NZ, pp. 479-484. cc_utas 260100 Geology Antarctica seismicity neotectonics tectonics lithosphere glacial isostatic adjustment Book Section PeerReviewed 2002 ftunivtasmania 2020-05-30T07:15:31Z A map of Antarctic intraplate earthquakes, 1900-99, is presented including records from the Global Seismic Network and recordings made at Antarctic seismic observatories and temporary stations. The results show a low but significant level of seismicity through the Transantarctic Mountains and across George V Land to Adelie Land. They also suggest some seismic deformation is taking place in the Antarctic Peninsula, Weddell Sea, East Antarctic coast, and Ross Sea. No globally recorded events have occurred in Marie Byrd Land to date. Local recordings across the continent show that a denser distribution of recording stations is needed before drawing conclusions from areas of apparent Antarctic aseismicity. This review is one of the first contributions to the SCAR-approved ANTEC initiative, which aims to co-ordinate work on neotectonic deformation across the continent. Book Part Adelie Land Antarc* Antarctic Antarctic Peninsula Antarctica George V Land Marie Byrd Land Ross Sea Weddell Sea University of Tasmania: UTas ePrints Antarctic Antarctic Peninsula Byrd George V Land ENVELOPE(148.000,148.000,-68.500,-68.500) Marie Byrd Land ENVELOPE(-130.000,-130.000,-78.000,-78.000) Ross Sea The Antarctic Transantarctic Mountains Weddell Weddell Sea
institution Open Polar
collection University of Tasmania: UTas ePrints
op_collection_id ftunivtasmania
language English
topic 260100 Geology
Antarctica
seismicity
neotectonics
tectonics
lithosphere
glacial isostatic adjustment
spellingShingle 260100 Geology
Antarctica
seismicity
neotectonics
tectonics
lithosphere
glacial isostatic adjustment
Reading, AM
Antarctic seismicity and neotectonics
topic_facet 260100 Geology
Antarctica
seismicity
neotectonics
tectonics
lithosphere
glacial isostatic adjustment
description A map of Antarctic intraplate earthquakes, 1900-99, is presented including records from the Global Seismic Network and recordings made at Antarctic seismic observatories and temporary stations. The results show a low but significant level of seismicity through the Transantarctic Mountains and across George V Land to Adelie Land. They also suggest some seismic deformation is taking place in the Antarctic Peninsula, Weddell Sea, East Antarctic coast, and Ross Sea. No globally recorded events have occurred in Marie Byrd Land to date. Local recordings across the continent show that a denser distribution of recording stations is needed before drawing conclusions from areas of apparent Antarctic aseismicity. This review is one of the first contributions to the SCAR-approved ANTEC initiative, which aims to co-ordinate work on neotectonic deformation across the continent.
author2 Gamble, J.A.
Skinner, D.N.B.
Henrys, S.
format Book Part
author Reading, AM
author_facet Reading, AM
author_sort Reading, AM
title Antarctic seismicity and neotectonics
title_short Antarctic seismicity and neotectonics
title_full Antarctic seismicity and neotectonics
title_fullStr Antarctic seismicity and neotectonics
title_full_unstemmed Antarctic seismicity and neotectonics
title_sort antarctic seismicity and neotectonics
publisher The Royal Society of New Zealand
publishDate 2002
url https://eprints.utas.edu.au/1875/
https://eprints.utas.edu.au/1875/1/Reading_2002_Antarctic_Seismicity_%26_Neotectonics.pdf
http://www.rsnz.org/publish/other/antarctica.php
long_lat ENVELOPE(148.000,148.000,-68.500,-68.500)
ENVELOPE(-130.000,-130.000,-78.000,-78.000)
geographic Antarctic
Antarctic Peninsula
Byrd
George V Land
Marie Byrd Land
Ross Sea
The Antarctic
Transantarctic Mountains
Weddell
Weddell Sea
geographic_facet Antarctic
Antarctic Peninsula
Byrd
George V Land
Marie Byrd Land
Ross Sea
The Antarctic
Transantarctic Mountains
Weddell
Weddell Sea
genre Adelie Land
Antarc*
Antarctic
Antarctic Peninsula
Antarctica
George V Land
Marie Byrd Land
Ross Sea
Weddell Sea
genre_facet Adelie Land
Antarc*
Antarctic
Antarctic Peninsula
Antarctica
George V Land
Marie Byrd Land
Ross Sea
Weddell Sea
op_relation https://eprints.utas.edu.au/1875/1/Reading_2002_Antarctic_Seismicity_%26_Neotectonics.pdf
Reading, AM orcid:0000-0002-9316-7605 2002 , 'Antarctic seismicity and neotectonics', in J.A. Gamble and D.N.B. Skinner and S. Henrys (eds.), Antarctica at the close of a millennium , Royal Society of New Zealand Bulletin, vol. 35 , The Royal Society of New Zealand, Wellington, NZ, pp. 479-484.
op_rights cc_utas
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