Review of global 2.1-1.8 Ga orogens: implications for a pre-Rodinia supercontinent
Available lithostratigraphic, tectonothermal, geochronological and paleomagnetic data from 2.1-1.8 Ga collisional orogens and related cratonic blocks around the world have established connections between South America and West Africa Western Australia and South Africa; Laurentia and Baltica; Siberia...
Main Authors: | , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2002
|
Subjects: | |
Online Access: | https://risweb.st-andrews.ac.uk/portal/en/researchoutput/review-of-global-2118-ga-orogens-implications-for-a-prerodinia-supercontinent(781ddf5c-2dfb-4730-94c3-de140d8e37e8).html http://www.scopus.com/inward/record.url?scp=0036851649&partnerID=8YFLogxK |
_version_ | 1821542738980503552 |
---|---|
author | Zhao, G C Cawood, Peter Anthony Wilde, S A Sun, M |
author_facet | Zhao, G C Cawood, Peter Anthony Wilde, S A Sun, M |
author_sort | Zhao, G C |
collection | University of St Andrews: Research Portal |
description | Available lithostratigraphic, tectonothermal, geochronological and paleomagnetic data from 2.1-1.8 Ga collisional orogens and related cratonic blocks around the world have established connections between South America and West Africa Western Australia and South Africa; Laurentia and Baltica; Siberia and Laurentia; Laurentia and Central Australia; East Antarctica and Laurentia, and North China and India. These links are interpreted to indicate the presence of a supercontinent existing before Rodinia, referred to herein as Columbia, a name recently proposed by Rogers and Santosh [Gondwana Res. 5 (2002) 5] for a Paleo-Mesoproterozoic supercontinent. In this supercontinent, the Archean to Paleoproterozoic cratonic blocks were welded by the global 2.1-1.8 Ga collisional belts. The cratonic blocks in South America and West Africa were welded by the 2.1-2.0 Ga Transamazonian and Eburnean Orogens; the KaapvaaI and Zimbabwe Cratons in southern Africa were collided along the similar to2.0 Ga Limpopo Belt; the cratonic blocks of Laurentia were sutured along the 1.9-1.8 Ga Trans-Hudson, Penokean, Taltson-Thelon, Wopmay, Ungava, Torngat and Nagssugtoqidian Orogens; the Kola, Karelia, Volgo-Uralia and Sarmatia (Ukrainian) Cratons in Baltica (Eastern Europe) were joined by the 1.9-1.8 Ga Kola-Karelia, Svecofennian, Volhyn-Central Russian and Pachelma Orogens; the Anabar and Aldan Cratons in Siberia were connected by the 1.9-1.8 Ga Akitkan and Central Aldan Orogens; the East Antarctica and an unknown confidential block were joined by the Transantarctic Mountains Orogen; the South and North Indian Blocks were amalgamated along the Central Indian Tectonic Zone; and the Eastern and Western Blocks of the North China Craton were welded together by the similar to1.85 Ga Trans-North China Orogen. The existence of Columbia is consistent with late Paleoproterozoic to Mesoproterozoic sedimentary and magmatic records. The similar to2.0 Ga fluvio-deltaic deposits have been found in all cratonic blocks in South America and West Africa, and ... |
format | Article in Journal/Newspaper |
genre | Antarc* Antarctica East Antarctica Siberia |
genre_facet | Antarc* Antarctica East Antarctica Siberia |
geographic | Aldan Anabar East Antarctica Hudson Indian Transantarctic Mountains Uralia |
geographic_facet | Aldan Anabar East Antarctica Hudson Indian Transantarctic Mountains Uralia |
id | ftunstandrewcris:oai:risweb.st-andrews.ac.uk:publications/781ddf5c-2dfb-4730-94c3-de140d8e37e8 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(129.546,129.546,63.447,63.447) ENVELOPE(113.624,113.624,73.286,73.286) ENVELOPE(6.967,6.967,62.608,62.608) |
op_collection_id | ftunstandrewcris |
op_rights | info:eu-repo/semantics/restrictedAccess |
op_source | Zhao , G C , Cawood , P A , Wilde , S A & Sun , M 2002 , ' Review of global 2.1-1.8 Ga orogens: implications for a pre-Rodinia supercontinent ' , Earth Science Reviews , vol. 59 , no. 1-4 , pp. 125-162 . |
publishDate | 2002 |
record_format | openpolar |
spelling | ftunstandrewcris:oai:risweb.st-andrews.ac.uk:publications/781ddf5c-2dfb-4730-94c3-de140d8e37e8 2025-01-16T19:03:49+00:00 Review of global 2.1-1.8 Ga orogens: implications for a pre-Rodinia supercontinent Zhao, G C Cawood, Peter Anthony Wilde, S A Sun, M 2002-11 https://risweb.st-andrews.ac.uk/portal/en/researchoutput/review-of-global-2118-ga-orogens-implications-for-a-prerodinia-supercontinent(781ddf5c-2dfb-4730-94c3-de140d8e37e8).html http://www.scopus.com/inward/record.url?scp=0036851649&partnerID=8YFLogxK eng eng info:eu-repo/semantics/restrictedAccess Zhao , G C , Cawood , P A , Wilde , S A & Sun , M 2002 , ' Review of global 2.1-1.8 Ga orogens: implications for a pre-Rodinia supercontinent ' , Earth Science Reviews , vol. 59 , no. 1-4 , pp. 125-162 . collisional orogen cratons Paleo-Mesoproterozoic supercontinent reconstruction NORTH CHINA CRATON TRANS-HUDSON OROGEN U-PB GEOCHRONOLOGY PALEOPROTEROZOIC TORNGAT-OROGEN NAGSSUGTOQIDIAN MOBILE BELT HIGH-PRESSURE GRANULITES WESTERN UNITED-STATES SINGLE ZIRCON AGES RIVER MAP AREA TECTONIC IMPLICATIONS article 2002 ftunstandrewcris 2021-12-26T14:17:48Z Available lithostratigraphic, tectonothermal, geochronological and paleomagnetic data from 2.1-1.8 Ga collisional orogens and related cratonic blocks around the world have established connections between South America and West Africa Western Australia and South Africa; Laurentia and Baltica; Siberia and Laurentia; Laurentia and Central Australia; East Antarctica and Laurentia, and North China and India. These links are interpreted to indicate the presence of a supercontinent existing before Rodinia, referred to herein as Columbia, a name recently proposed by Rogers and Santosh [Gondwana Res. 5 (2002) 5] for a Paleo-Mesoproterozoic supercontinent. In this supercontinent, the Archean to Paleoproterozoic cratonic blocks were welded by the global 2.1-1.8 Ga collisional belts. The cratonic blocks in South America and West Africa were welded by the 2.1-2.0 Ga Transamazonian and Eburnean Orogens; the KaapvaaI and Zimbabwe Cratons in southern Africa were collided along the similar to2.0 Ga Limpopo Belt; the cratonic blocks of Laurentia were sutured along the 1.9-1.8 Ga Trans-Hudson, Penokean, Taltson-Thelon, Wopmay, Ungava, Torngat and Nagssugtoqidian Orogens; the Kola, Karelia, Volgo-Uralia and Sarmatia (Ukrainian) Cratons in Baltica (Eastern Europe) were joined by the 1.9-1.8 Ga Kola-Karelia, Svecofennian, Volhyn-Central Russian and Pachelma Orogens; the Anabar and Aldan Cratons in Siberia were connected by the 1.9-1.8 Ga Akitkan and Central Aldan Orogens; the East Antarctica and an unknown confidential block were joined by the Transantarctic Mountains Orogen; the South and North Indian Blocks were amalgamated along the Central Indian Tectonic Zone; and the Eastern and Western Blocks of the North China Craton were welded together by the similar to1.85 Ga Trans-North China Orogen. The existence of Columbia is consistent with late Paleoproterozoic to Mesoproterozoic sedimentary and magmatic records. The similar to2.0 Ga fluvio-deltaic deposits have been found in all cratonic blocks in South America and West Africa, and ... Article in Journal/Newspaper Antarc* Antarctica East Antarctica Siberia University of St Andrews: Research Portal Aldan ENVELOPE(129.546,129.546,63.447,63.447) Anabar ENVELOPE(113.624,113.624,73.286,73.286) East Antarctica Hudson Indian Transantarctic Mountains Uralia ENVELOPE(6.967,6.967,62.608,62.608) |
spellingShingle | collisional orogen cratons Paleo-Mesoproterozoic supercontinent reconstruction NORTH CHINA CRATON TRANS-HUDSON OROGEN U-PB GEOCHRONOLOGY PALEOPROTEROZOIC TORNGAT-OROGEN NAGSSUGTOQIDIAN MOBILE BELT HIGH-PRESSURE GRANULITES WESTERN UNITED-STATES SINGLE ZIRCON AGES RIVER MAP AREA TECTONIC IMPLICATIONS Zhao, G C Cawood, Peter Anthony Wilde, S A Sun, M Review of global 2.1-1.8 Ga orogens: implications for a pre-Rodinia supercontinent |
title | Review of global 2.1-1.8 Ga orogens: implications for a pre-Rodinia supercontinent |
title_full | Review of global 2.1-1.8 Ga orogens: implications for a pre-Rodinia supercontinent |
title_fullStr | Review of global 2.1-1.8 Ga orogens: implications for a pre-Rodinia supercontinent |
title_full_unstemmed | Review of global 2.1-1.8 Ga orogens: implications for a pre-Rodinia supercontinent |
title_short | Review of global 2.1-1.8 Ga orogens: implications for a pre-Rodinia supercontinent |
title_sort | review of global 2.1-1.8 ga orogens: implications for a pre-rodinia supercontinent |
topic | collisional orogen cratons Paleo-Mesoproterozoic supercontinent reconstruction NORTH CHINA CRATON TRANS-HUDSON OROGEN U-PB GEOCHRONOLOGY PALEOPROTEROZOIC TORNGAT-OROGEN NAGSSUGTOQIDIAN MOBILE BELT HIGH-PRESSURE GRANULITES WESTERN UNITED-STATES SINGLE ZIRCON AGES RIVER MAP AREA TECTONIC IMPLICATIONS |
topic_facet | collisional orogen cratons Paleo-Mesoproterozoic supercontinent reconstruction NORTH CHINA CRATON TRANS-HUDSON OROGEN U-PB GEOCHRONOLOGY PALEOPROTEROZOIC TORNGAT-OROGEN NAGSSUGTOQIDIAN MOBILE BELT HIGH-PRESSURE GRANULITES WESTERN UNITED-STATES SINGLE ZIRCON AGES RIVER MAP AREA TECTONIC IMPLICATIONS |
url | https://risweb.st-andrews.ac.uk/portal/en/researchoutput/review-of-global-2118-ga-orogens-implications-for-a-prerodinia-supercontinent(781ddf5c-2dfb-4730-94c3-de140d8e37e8).html http://www.scopus.com/inward/record.url?scp=0036851649&partnerID=8YFLogxK |