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Middle Paleozoic convergent orogenic belts in western Inner Mongolia (China): framework, kinematics, geochronology and implications for tectonic evolution of the Central Asian Orogenic Belt

TLDR
Based mainly on field geological observation and geochronologic data, six tectonic units have been recognized in western Inner Mongolia (China), including, from south to north: North China Craton (NCC), Southern Orogenic Belt (SOB), Hunshandake Block (HB), Northern Orogenics Belt (NOB), South Mongolia microcontinent (SMM), and Southern margin of Ergun Block (SME), suggesting that the Tectonic framework of the CAOB is characterized by an accretion of different blocks and orogenic belts RE
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This article is published in Gondwana Research.The article was published on 2013-05-01 and is currently open access. It has received 441 citations till now. The article focuses on the topics: Foreland basin & Craton.

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A Tale of Amalgamation of Three Permo-Triassic Collage Systems in Central Asia: Oroclines, Sutures, and Terminal Accretion

TL;DR: The Central Asian Orogenic Belt as discussed by the authors 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 orogine was formed.
Journal ArticleDOI

Introduction to tectonics of China

TL;DR: In the last three decades, extensive geological, geochemical and geophysical investigations have been carried out on these cratonic blocks and intervening orogenic belts, producing an abundant amount of new data and competing interpretations.
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Final closure of the Paleo‐Asian Ocean along the Solonker Suture Zone: Constraints from geochronological and geochemical data of Permian volcanic and sedimentary rocks

TL;DR: In this article, provenance analysis of Permian sedimentary rocks of arc basins along the Xar Moron River was carried out, which revealed a close relationship between the sedimentary and volcanic rock suite in the study region suggesting short transport distances and a complex convergent arc setting.
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Final amalgamation of the Tianshan and Junggar orogenic collage in the southwestern Central Asian Orogenic Belt: Constraints on the closure of the Paleo-Asian Ocean

TL;DR: The Tianshan and Junggar orogenic collage occupied the southwestern part of the Central Asian Orogenic Belt and was assembled by collision/accretion of several continental blocks and island arcs during late Paleozoic-early Mesozoic time.
References
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Journal ArticleDOI

Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry

TL;DR: In this paper, laser ablation-inductively coupled plasma-mass spectrometry was used for age determination of zircons of Proterozoic to Oligocene ages (1060-31 Ma).
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Granitoids of the Central Asian Orogenic Belt and Continental Growth in the Phanerozoic

TL;DR: Most Phanerozoic granitoids of Central Asia are characterised by low initial Sr isotopic ratios, positive eNd(T) values and young Sm-Nd model ages (TDM) of 300-1200 Ma.
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A new terrane subdivision for Mongolia: implications for the Phanerozoic crustal growth of Central Asia

TL;DR: In this article, the authors present a new terrane synthesis for Mongolia that incorporates geological, geochemical and geochronological data from more than 60 years of Mongolian, Russian and joint international studies, which can provide an important crustal framework for interpreting the Phanerozoic tectonic evolution of a large part of Central Asia.
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