Consistent kinematic architecture in the damage zones of intraplate strike-slip fault systems in North Victoria Land, Antarctica and implications for fault zone evolution RID C-1391-2009
Cumulative, polymodal normal (Gaussian distribution) statistics was applied to subsidiary fault data collected from damage zones associated with the Cenozoic Lanterman and Priestley intraplate right-lateral strike-slip fault systems in North Victoria Land, Antarctica. Results show that five Gaussian...
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ftunivroma3iris:oai:iris.uniroma3.it:11590/136129 2024-02-27T08:33:22+00:00 Consistent kinematic architecture in the damage zones of intraplate strike-slip fault systems in North Victoria Land, Antarctica and implications for fault zone evolution RID C-1391-2009 Storti F Laufer AL ROSSETTI, FEDERICO SALVINI, Francesco Storti, F Rossetti, Federico Laufer, Al Salvini, Francesco 2006 http://hdl.handle.net/11590/136129 https://doi.org/10.1016/j.jsg.2005.09.004 eng eng info:eu-repo/semantics/altIdentifier/wos/WOS:000235153800005 volume:28 issue:1 firstpage:50 lastpage:63 numberofpages:14 journal:JOURNAL OF STRUCTURAL GEOLOGY http://hdl.handle.net/11590/136129 doi:10.1016/j.jsg.2005.09.004 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-31144466036 Subsidiary fault Paleostre Antarctica info:eu-repo/semantics/article 2006 ftunivroma3iris https://doi.org/10.1016/j.jsg.2005.09.004 2024-01-31T17:36:42Z Cumulative, polymodal normal (Gaussian distribution) statistics was applied to subsidiary fault data collected from damage zones associated with the Cenozoic Lanterman and Priestley intraplate right-lateral strike-slip fault systems in North Victoria Land, Antarctica. Results show that five Gaussian peaks out of seven in the Lanterman Fault and five out of nine in the Priestley Fault have almost coincident azimuthal values. We named these Gaussian peak pairs as consistent fault sets, arranged in a consistent kinematic architecture that is compatible with the Cenozoic regional strike-slip environment. Angular and kinematic relationships among subsidiary fault sets within the consistent kinematic architecture provide constraints for the inference of the state of stress along the Lanterman and Priestley fault systems. We interpret the fault pattern of the consistent kinematic architecture to be produced by early localisation of the principal displacement zone along pre-existing mechanical discontinuities inherited from the Early Paleozoic Ross Orogeny. Shear localisation was followed by subsidiary faulting at an angle to the principal displacement zone according to the Mohr–Coulomb–Byerlee failure criterion. Article in Journal/Newspaper Antarc* Antarctica Victoria Land Anagrafe della Ricerca d'Ateneo (Universitá degli studi Roma Tre) Victoria Land Priestley ENVELOPE(161.883,161.883,-75.183,-75.183) Journal of Structural Geology 28 1 50 63 |
institution |
Open Polar |
collection |
Anagrafe della Ricerca d'Ateneo (Universitá degli studi Roma Tre) |
op_collection_id |
ftunivroma3iris |
language |
English |
topic |
Subsidiary fault Paleostre Antarctica |
spellingShingle |
Subsidiary fault Paleostre Antarctica Storti F Laufer AL ROSSETTI, FEDERICO SALVINI, Francesco Consistent kinematic architecture in the damage zones of intraplate strike-slip fault systems in North Victoria Land, Antarctica and implications for fault zone evolution RID C-1391-2009 |
topic_facet |
Subsidiary fault Paleostre Antarctica |
description |
Cumulative, polymodal normal (Gaussian distribution) statistics was applied to subsidiary fault data collected from damage zones associated with the Cenozoic Lanterman and Priestley intraplate right-lateral strike-slip fault systems in North Victoria Land, Antarctica. Results show that five Gaussian peaks out of seven in the Lanterman Fault and five out of nine in the Priestley Fault have almost coincident azimuthal values. We named these Gaussian peak pairs as consistent fault sets, arranged in a consistent kinematic architecture that is compatible with the Cenozoic regional strike-slip environment. Angular and kinematic relationships among subsidiary fault sets within the consistent kinematic architecture provide constraints for the inference of the state of stress along the Lanterman and Priestley fault systems. We interpret the fault pattern of the consistent kinematic architecture to be produced by early localisation of the principal displacement zone along pre-existing mechanical discontinuities inherited from the Early Paleozoic Ross Orogeny. Shear localisation was followed by subsidiary faulting at an angle to the principal displacement zone according to the Mohr–Coulomb–Byerlee failure criterion. |
author2 |
Storti, F Rossetti, Federico Laufer, Al Salvini, Francesco |
format |
Article in Journal/Newspaper |
author |
Storti F Laufer AL ROSSETTI, FEDERICO SALVINI, Francesco |
author_facet |
Storti F Laufer AL ROSSETTI, FEDERICO SALVINI, Francesco |
author_sort |
Storti F |
title |
Consistent kinematic architecture in the damage zones of intraplate strike-slip fault systems in North Victoria Land, Antarctica and implications for fault zone evolution RID C-1391-2009 |
title_short |
Consistent kinematic architecture in the damage zones of intraplate strike-slip fault systems in North Victoria Land, Antarctica and implications for fault zone evolution RID C-1391-2009 |
title_full |
Consistent kinematic architecture in the damage zones of intraplate strike-slip fault systems in North Victoria Land, Antarctica and implications for fault zone evolution RID C-1391-2009 |
title_fullStr |
Consistent kinematic architecture in the damage zones of intraplate strike-slip fault systems in North Victoria Land, Antarctica and implications for fault zone evolution RID C-1391-2009 |
title_full_unstemmed |
Consistent kinematic architecture in the damage zones of intraplate strike-slip fault systems in North Victoria Land, Antarctica and implications for fault zone evolution RID C-1391-2009 |
title_sort |
consistent kinematic architecture in the damage zones of intraplate strike-slip fault systems in north victoria land, antarctica and implications for fault zone evolution rid c-1391-2009 |
publishDate |
2006 |
url |
http://hdl.handle.net/11590/136129 https://doi.org/10.1016/j.jsg.2005.09.004 |
long_lat |
ENVELOPE(161.883,161.883,-75.183,-75.183) |
geographic |
Victoria Land Priestley |
geographic_facet |
Victoria Land Priestley |
genre |
Antarc* Antarctica Victoria Land |
genre_facet |
Antarc* Antarctica Victoria Land |
op_relation |
info:eu-repo/semantics/altIdentifier/wos/WOS:000235153800005 volume:28 issue:1 firstpage:50 lastpage:63 numberofpages:14 journal:JOURNAL OF STRUCTURAL GEOLOGY http://hdl.handle.net/11590/136129 doi:10.1016/j.jsg.2005.09.004 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-31144466036 |
op_doi |
https://doi.org/10.1016/j.jsg.2005.09.004 |
container_title |
Journal of Structural Geology |
container_volume |
28 |
container_issue |
1 |
container_start_page |
50 |
op_container_end_page |
63 |
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1792045248578322432 |