THE LATE PALEOZOIC EVOLUTION OF THE CENTRAL INNER MONGOLIA, CHINA: A PERSPECTIVE FROM METAMORPHIC STUDY

The Xing’an-Inner Mongolia Orogenic Belt (XIMOB) exposed in the eastern section of the Central Asian Orogenic Belt (CAOB) is generally thought to have resulted from closure of the Paleo-Asian ocean [Şengör et al., 1993]. However, the current hot debate is focused on whether the orogen formed through...

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Main Authors: J. R. Zhang, C. J. Wei, H. Chu, Y. P. Chen
Format: Article
Language:English
Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2017-09-01
Series:Геодинамика и тектонофизика
Online Access:https://www.gt-crust.ru/jour/article/view/447
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author J. R. Zhang
C. J. Wei
H. Chu
Y. P. Chen
author_facet J. R. Zhang
C. J. Wei
H. Chu
Y. P. Chen
author_sort J. R. Zhang
collection DOAJ
description The Xing’an-Inner Mongolia Orogenic Belt (XIMOB) exposed in the eastern section of the Central Asian Orogenic Belt (CAOB) is generally thought to have resulted from closure of the Paleo-Asian ocean [Şengör et al., 1993]. However, the current hot debate is focused on whether the orogen formed through continuous subduction and accretion over a prolonged period of time until the closure of the Paleo-Asian ocean at the Early Triassic [Xiao et al., 2003], or through the subduction of the Paleo-Asian ocean and related collision in the Early-Mid Devonian [Xu et al., 2013], and the tectonic setting in the Late Paleozoic to Mesozoic has been a pivotal issue.
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institution Kabale University
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publishDate 2017-09-01
publisher Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
record_format Article
series Геодинамика и тектонофизика
spelling doaj-art-ee58f6f5d9074844b05feeec1b5de8b82025-08-20T03:37:06ZengRussian Academy of Sciences, Siberian Branch, Institute of the Earth's crustГеодинамика и тектонофизика2078-502X2017-09-018360961110.5800/GT-2017-8-3-0306306THE LATE PALEOZOIC EVOLUTION OF THE CENTRAL INNER MONGOLIA, CHINA: A PERSPECTIVE FROM METAMORPHIC STUDYJ. R. Zhang0C. J. Wei1H. Chu2Y. P. Chen3School of Earth and Space Sciences, Peking UniversitySchool of Earth and Space Sciences, Peking UniversityTianjin Institute of Geology and Mineral ResourcesSchool of Earth and Space Sciences, Peking UniversityThe Xing’an-Inner Mongolia Orogenic Belt (XIMOB) exposed in the eastern section of the Central Asian Orogenic Belt (CAOB) is generally thought to have resulted from closure of the Paleo-Asian ocean [Şengör et al., 1993]. However, the current hot debate is focused on whether the orogen formed through continuous subduction and accretion over a prolonged period of time until the closure of the Paleo-Asian ocean at the Early Triassic [Xiao et al., 2003], or through the subduction of the Paleo-Asian ocean and related collision in the Early-Mid Devonian [Xu et al., 2013], and the tectonic setting in the Late Paleozoic to Mesozoic has been a pivotal issue.https://www.gt-crust.ru/jour/article/view/447
spellingShingle J. R. Zhang
C. J. Wei
H. Chu
Y. P. Chen
THE LATE PALEOZOIC EVOLUTION OF THE CENTRAL INNER MONGOLIA, CHINA: A PERSPECTIVE FROM METAMORPHIC STUDY
Геодинамика и тектонофизика
title THE LATE PALEOZOIC EVOLUTION OF THE CENTRAL INNER MONGOLIA, CHINA: A PERSPECTIVE FROM METAMORPHIC STUDY
title_full THE LATE PALEOZOIC EVOLUTION OF THE CENTRAL INNER MONGOLIA, CHINA: A PERSPECTIVE FROM METAMORPHIC STUDY
title_fullStr THE LATE PALEOZOIC EVOLUTION OF THE CENTRAL INNER MONGOLIA, CHINA: A PERSPECTIVE FROM METAMORPHIC STUDY
title_full_unstemmed THE LATE PALEOZOIC EVOLUTION OF THE CENTRAL INNER MONGOLIA, CHINA: A PERSPECTIVE FROM METAMORPHIC STUDY
title_short THE LATE PALEOZOIC EVOLUTION OF THE CENTRAL INNER MONGOLIA, CHINA: A PERSPECTIVE FROM METAMORPHIC STUDY
title_sort late paleozoic evolution of the central inner mongolia china a perspective from metamorphic study
url https://www.gt-crust.ru/jour/article/view/447
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