Stratigraphic landscape analysis, thermochronology and the episodic development of elevated, passive continental margins
The continental margin of West Greenland is similar in many respects to other elevated, passive continental margins (EPCMs) around the world. These margins are characterised by extensive regions of low relief at elevations of 1–2 kilometres above sea level sloping gently inland, with a much steeper,...
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Geological Survey of Denmark and Greenland
2013
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ftdoajarticles:oai:doaj.org/article:61cf2e55df2a416198fb7f13036e40a8 2023-05-15T16:27:19+02:00 Stratigraphic landscape analysis, thermochronology and the episodic development of elevated, passive continental margins Green, Paul F. Lidmar-Bergsteröm, K. Japsen, Peter Bonow, J.M. Chalmers, J.M. 2013-12-01T00:00:00Z https://doaj.org/article/61cf2e55df2a416198fb7f13036e40a8 EN eng Geological Survey of Denmark and Greenland http://www.geus.dk/DK/publications/geol-survey-dk-gl-bull/30/Documents/nr30_p001-150.pdf https://doaj.org/toc/1604-8156 1604-8156 https://doaj.org/article/61cf2e55df2a416198fb7f13036e40a8 Geological Survey of Denmark and Greenland Bulletin, Vol 30, Pp 1-150 (2013) Apatite fission-track analysis base level continental margins denudation geomorphology Great Escarpment peneplain stratigraphic landscape analysis thermochronology uplift Geology QE1-996.5 Geophysics. Cosmic physics QC801-809 article 2013 ftdoajarticles 2022-12-31T08:33:13Z The continental margin of West Greenland is similar in many respects to other elevated, passive continental margins (EPCMs) around the world. These margins are characterised by extensive regions of low relief at elevations of 1–2 kilometres above sea level sloping gently inland, with a much steeper, oceanward decline, often termed a 'Great Escarpment', terminating at a coastal plain. Recent studies, based on integration of geological, geomorphological and thermochronological evidence, have shown that the high topography of West Greenland was formed by differential uplift and dissection of an Oligo-Miocene peneplain since the late Miocene, many millions of years after continental break-up between Greenland and North America. In contrast, many studies of other EPCMs have proposed a different style of development in which the high plateaux and the steep, oceanward decline are regarded as a direct result of rifting and continental separation. Some studies assume that the elevated regions have remained high since break-up, with the high topography continuously renewed by isostasy. Others identify the elevated plains as remnants of pre-rift landscapes. Key to understanding the development of the West Greenland margin is a new approach to the study of landforms, stratigraphic landscape analysis, in which the low-relief, high-elevation plateaux at EPCMs are interpreted as uplifted peneplains: low-relief surfaces of large extent, cutting across bedrock of different age and resistance, and originally graded to sea level. Identification of different generations of peneplain (re-exposed and epigene) from regional mapping, combined with geological constraints and thermochronology, allows definition of the evolution leading to the formation of the modern-day topography. This approach is founded particularly on results from the South Swedish Dome, which document former sea levels as base levels for the formation of peneplains. These results support the view that peneplains grade towards base level, and that in the absence of ... Article in Journal/Newspaper Greenland Geological Survey of Denmark and Greenland Bulletin Directory of Open Access Journals: DOAJ Articles Greenland |
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Directory of Open Access Journals: DOAJ Articles |
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English |
topic |
Apatite fission-track analysis base level continental margins denudation geomorphology Great Escarpment peneplain stratigraphic landscape analysis thermochronology uplift Geology QE1-996.5 Geophysics. Cosmic physics QC801-809 |
spellingShingle |
Apatite fission-track analysis base level continental margins denudation geomorphology Great Escarpment peneplain stratigraphic landscape analysis thermochronology uplift Geology QE1-996.5 Geophysics. Cosmic physics QC801-809 Green, Paul F. Lidmar-Bergsteröm, K. Japsen, Peter Bonow, J.M. Chalmers, J.M. Stratigraphic landscape analysis, thermochronology and the episodic development of elevated, passive continental margins |
topic_facet |
Apatite fission-track analysis base level continental margins denudation geomorphology Great Escarpment peneplain stratigraphic landscape analysis thermochronology uplift Geology QE1-996.5 Geophysics. Cosmic physics QC801-809 |
description |
The continental margin of West Greenland is similar in many respects to other elevated, passive continental margins (EPCMs) around the world. These margins are characterised by extensive regions of low relief at elevations of 1–2 kilometres above sea level sloping gently inland, with a much steeper, oceanward decline, often termed a 'Great Escarpment', terminating at a coastal plain. Recent studies, based on integration of geological, geomorphological and thermochronological evidence, have shown that the high topography of West Greenland was formed by differential uplift and dissection of an Oligo-Miocene peneplain since the late Miocene, many millions of years after continental break-up between Greenland and North America. In contrast, many studies of other EPCMs have proposed a different style of development in which the high plateaux and the steep, oceanward decline are regarded as a direct result of rifting and continental separation. Some studies assume that the elevated regions have remained high since break-up, with the high topography continuously renewed by isostasy. Others identify the elevated plains as remnants of pre-rift landscapes. Key to understanding the development of the West Greenland margin is a new approach to the study of landforms, stratigraphic landscape analysis, in which the low-relief, high-elevation plateaux at EPCMs are interpreted as uplifted peneplains: low-relief surfaces of large extent, cutting across bedrock of different age and resistance, and originally graded to sea level. Identification of different generations of peneplain (re-exposed and epigene) from regional mapping, combined with geological constraints and thermochronology, allows definition of the evolution leading to the formation of the modern-day topography. This approach is founded particularly on results from the South Swedish Dome, which document former sea levels as base levels for the formation of peneplains. These results support the view that peneplains grade towards base level, and that in the absence of ... |
format |
Article in Journal/Newspaper |
author |
Green, Paul F. Lidmar-Bergsteröm, K. Japsen, Peter Bonow, J.M. Chalmers, J.M. |
author_facet |
Green, Paul F. Lidmar-Bergsteröm, K. Japsen, Peter Bonow, J.M. Chalmers, J.M. |
author_sort |
Green, Paul F. |
title |
Stratigraphic landscape analysis, thermochronology and the episodic development of elevated, passive continental margins |
title_short |
Stratigraphic landscape analysis, thermochronology and the episodic development of elevated, passive continental margins |
title_full |
Stratigraphic landscape analysis, thermochronology and the episodic development of elevated, passive continental margins |
title_fullStr |
Stratigraphic landscape analysis, thermochronology and the episodic development of elevated, passive continental margins |
title_full_unstemmed |
Stratigraphic landscape analysis, thermochronology and the episodic development of elevated, passive continental margins |
title_sort |
stratigraphic landscape analysis, thermochronology and the episodic development of elevated, passive continental margins |
publisher |
Geological Survey of Denmark and Greenland |
publishDate |
2013 |
url |
https://doaj.org/article/61cf2e55df2a416198fb7f13036e40a8 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Geological Survey of Denmark and Greenland Bulletin |
genre_facet |
Greenland Geological Survey of Denmark and Greenland Bulletin |
op_source |
Geological Survey of Denmark and Greenland Bulletin, Vol 30, Pp 1-150 (2013) |
op_relation |
http://www.geus.dk/DK/publications/geol-survey-dk-gl-bull/30/Documents/nr30_p001-150.pdf https://doaj.org/toc/1604-8156 1604-8156 https://doaj.org/article/61cf2e55df2a416198fb7f13036e40a8 |
_version_ |
1766016457989160960 |