A Tale of Amalgamation of Three Permo-Triassic Collage Systems in Central Asia: Oroclines, Sutures, and Terminal Accretion
The Central Asian Orogenic Belt records the accretion and convergence of three collage systems that were finally rotated into two major oroclines. The Mongolia collage system was a long, N-S-oriented composite ribbon that was rotated to its current orientation when the Mongol-Okhotsk orocline was fo...
Ausführliche Beschreibung
Autor*in: |
Wenjiao Xiao [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
2015 |
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Rechteinformationen: |
Nutzungsrecht: © COPYRIGHT 2015 Annual Reviews, Inc. |
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Schlagwörter: |
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Übergeordnetes Werk: |
Enthalten in: Annual review of earth and planetary sciences - Palo Alto, Calif. : Annual Reviews Inc., 1973, 43(2015), Seite 477 |
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Übergeordnetes Werk: |
volume:43 ; year:2015 ; pages:477 |
Links: |
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DOI / URN: |
10.1146/annurev-earth-060614-105254 |
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10.1146/annurev-earth-060614-105254 doi PQ20160617 (DE-627)OLC1967206015 (DE-599)GBVOLC1967206015 (PRQ)g1637-b6f269ed3979d88b232f5649790f1f0f2f6ec5632e96a9d5476d81080d9404c70 (KEY)0070005320150000043000000477taleofamalgamationofthreepermotriassiccollagesyste DE-627 ger DE-627 rakwb eng 550 ZDB 38.00 bkl 39.53 bkl Wenjiao Xiao verfasserin aut A Tale of Amalgamation of Three Permo-Triassic Collage Systems in Central Asia: Oroclines, Sutures, and Terminal Accretion 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The Central Asian Orogenic Belt records the accretion and convergence of three collage systems that were finally rotated into two major oroclines. The Mongolia collage system was a long, N-S-oriented composite ribbon that was rotated to its current orientation when the Mongol-Okhotsk orocline was formed. The components of the Kazakhstan collage system were welded together into a long, single composite arc that was bent to form the Kazakhstan orocline. The cratons of Tarim and North China were united and sutured by the Beishan orogen, which terminated with formation of the Solonker suture in northern China. All components of the three collage systems were generated by the Neoproterozoic and were amalgamated in the Permo-Triassic. The Central Asian Orogenic Belt evolved by multiple convergence and accretion of many orogenic components during multiple phases of amalgamation, followed by two phases of orocline rotation. Nutzungsrecht: © COPYRIGHT 2015 Annual Reviews, Inc. Continental dynamics Plate tectonics Geomorphology China Central Asia Mongolia Brian F Windley oth Shu Sun oth Jiliang Li oth Baochun Huang oth Chunming Han oth Chao Yuan oth Min Sun oth Hanlin Chen oth Enthalten in Annual review of earth and planetary sciences Palo Alto, Calif. : Annual Reviews Inc., 1973 43(2015), Seite 477 (DE-627)129307920 (DE-600)124813-3 (DE-576)014506491 0084-6597 nnns volume:43 year:2015 pages:477 http://dx.doi.org/10.1146/annurev-earth-060614-105254 Volltext http://search.proquest.com/docview/1689330558 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-AST SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_70 GBV_ILN_2012 GBV_ILN_2027 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 38.00 AVZ 39.53 AVZ AR 43 2015 477 |
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550 ZDB 38.00 bkl 39.53 bkl A Tale of Amalgamation of Three Permo-Triassic Collage Systems in Central Asia: Oroclines, Sutures, and Terminal Accretion Continental dynamics Plate tectonics Geomorphology China Central Asia Mongolia |
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A Tale of Amalgamation of Three Permo-Triassic Collage Systems in Central Asia: Oroclines, Sutures, and Terminal Accretion |
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A Tale of Amalgamation of Three Permo-Triassic Collage Systems in Central Asia: Oroclines, Sutures, and Terminal Accretion |
abstract |
The Central Asian Orogenic Belt records the accretion and convergence of three collage systems that were finally rotated into two major oroclines. The Mongolia collage system was a long, N-S-oriented composite ribbon that was rotated to its current orientation when the Mongol-Okhotsk orocline was formed. The components of the Kazakhstan collage system were welded together into a long, single composite arc that was bent to form the Kazakhstan orocline. The cratons of Tarim and North China were united and sutured by the Beishan orogen, which terminated with formation of the Solonker suture in northern China. All components of the three collage systems were generated by the Neoproterozoic and were amalgamated in the Permo-Triassic. The Central Asian Orogenic Belt evolved by multiple convergence and accretion of many orogenic components during multiple phases of amalgamation, followed by two phases of orocline rotation. |
abstractGer |
The Central Asian Orogenic Belt records the accretion and convergence of three collage systems that were finally rotated into two major oroclines. The Mongolia collage system was a long, N-S-oriented composite ribbon that was rotated to its current orientation when the Mongol-Okhotsk orocline was formed. The components of the Kazakhstan collage system were welded together into a long, single composite arc that was bent to form the Kazakhstan orocline. The cratons of Tarim and North China were united and sutured by the Beishan orogen, which terminated with formation of the Solonker suture in northern China. All components of the three collage systems were generated by the Neoproterozoic and were amalgamated in the Permo-Triassic. The Central Asian Orogenic Belt evolved by multiple convergence and accretion of many orogenic components during multiple phases of amalgamation, followed by two phases of orocline rotation. |
abstract_unstemmed |
The Central Asian Orogenic Belt records the accretion and convergence of three collage systems that were finally rotated into two major oroclines. The Mongolia collage system was a long, N-S-oriented composite ribbon that was rotated to its current orientation when the Mongol-Okhotsk orocline was formed. The components of the Kazakhstan collage system were welded together into a long, single composite arc that was bent to form the Kazakhstan orocline. The cratons of Tarim and North China were united and sutured by the Beishan orogen, which terminated with formation of the Solonker suture in northern China. All components of the three collage systems were generated by the Neoproterozoic and were amalgamated in the Permo-Triassic. The Central Asian Orogenic Belt evolved by multiple convergence and accretion of many orogenic components during multiple phases of amalgamation, followed by two phases of orocline rotation. |
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title_short |
A Tale of Amalgamation of Three Permo-Triassic Collage Systems in Central Asia: Oroclines, Sutures, and Terminal Accretion |
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