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Journal ArticleDOI

Gondwana from top to base in space and time

TLDR
Gondwana is reviewed from the unification of its several cratons in the Late Neoproterozoic, through its combination with Laurussia in the Carboniferous to form Pangea and up to its progressive fragmentation in the Mesozoic.
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This article is published in Gondwana Research.The article was published on 2013-11-01. It has received 460 citations till now. The article focuses on the topics: Gondwana & Paleozoic.

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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.
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The western Central Asian Orogenic Belt: A window to accretionary orogenesis and continental growth

TL;DR: An overview of the orogenic components and their amalgamation in the western Central Asian Orogenic Belt (CAOB) is presented in this paper, which records the convergence and interactions among various types of orogens including the Japan-type, Mariana-type and Alaska-Aleutian-type arc systems, as well as the active marginal sequences of the Siberia Craton, which incorporated wide accretionary complexes and accreted arcs and terranes.
Journal ArticleDOI

Geological reconstructions of the East Asian blocks: From the breakup of Rodinia to the assembly of Pangea

TL;DR: In this paper, the authors carried out geological and paleomagnetic investigations on East Asian blocks and associated orogenic belts, supported by a NSFC Major Program entitled “Reconstructions of East Asian Blocks in Pangea”.
Journal ArticleDOI

Plate tectonics in the late Paleozoic

TL;DR: In this article, a model for the late Paleozoic (410-250 million years ago) is presented, together with a review of the underlying data, which can be used for numerical mantle modeling, and serve as a general framework for understanding late paleozoic tectonics.
Book

Earth History and Palaeogeography

TL;DR: Using full-colour palaeogeographical maps from the Cambrian to the present, this interdisciplinary volume explains how plate motions and surface volcanism are linked to processes in the Earth's mantle, and to climate change and the evolution of Earth's biota.
References
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Global continental and ocean basin reconstructions since 200 Ma

TL;DR: In this paper, a new type of global plate motion model consisting of a set of continuously-closing topological plate polygons with associated plate boundaries and plate velocities since the break-up of the supercontinent Pangea is presented.
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Gondwana dispersion and Asian accretion: Tectonic and palaeogeographic evolution of eastern Tethys

TL;DR: The Phanerozoic evolution of the region is the result of more than 400 million years of continental dispersion from Gondwana and plate tectonic convergence, collision and accretion as discussed by the authors.
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Phanerozoic polar wander, palaeogeography and dynamics

TL;DR: A significant number of new palaeomagnetic poles have become available since the last time a compilation was made (assembled in 2005, published in 2008) to indicate to us that a new and significantly expanded set of tables with palaeOMagnetic results would be valuable, with results coming from the Gondwana cratonic elements, Laurentia, Baltica/Europe, and Siberia as mentioned in this paper.
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