Palaeozoic accretionary and convergent tectonics of the southern Altaids; implications for the growth of Central Asia

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doi: 10.1144/0016-764903-165
Authors:Xiao, W.; Windley, B. F.; Badarch, G.; Sun, S.; Li, J.; Qin, K.; Wang, Z.
Author Affiliations:Primary:
Chinese Academy of Sciences, Institute of Geology and Geophysics, Beijing, China
Other:
University of Leicester, United Kingdom
Mongolian Academy of Sciences, Mongolia
Volume Title:Journal of the Geological Society of London
Source:Journal of the Geological Society of London, 161(3), p.339-342. Publisher: Geological Society of London, London, United Kingdom. ISSN: 0016-7649
Publication Date:2004
Note:In English. 27 refs.; illus., incl. sects., 1 table, geol. sketch map
Summary:The southern Altaids present a unidirectional section from Mongolia to China through an accretionary orogen that youngs progressively from Neoproterozoic in the north to Permian in the south. The orogen formed by forearc accretion of island arcs, accretionary wedges, ophiolites and Precambrian microcontinents. This regularity was upset by early growth within the ocean of arcs that later collided at the accreting continental margin, by imbrication of old ophiolites with young arcs, and by Himalayan-style thrust-nappe tectonics when an arc collided into a microcontinent. Lateral growth of the Southern Altaids represents a massive addition of juvenile material to the Palaeozoic crust.
Sections:Petrology
Subsections:General
Subjects:Accreting plate boundary; Accretionary wedges; Basins; Crust; Faults; Fore-arc basins; Imbricate tectonics; Island arcs; Metamorphic rocks; Nappes; Ophiolite; Orogenic belts; Paleozoic; Plate collision; Plate convergence; Plate tectonics; Subduction; Tectonics; Tectonostratigraphic units; Thrust faults; Altai Mountains; Asia; Central Asia; China; Far East; Junggar; Mongolia; Xinjiang China
Coordinates:N443000 N483000 E0933000 E0880000
Abstract Numbers:04M/1930
Record ID:2004051475
Copyright Information:GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from The Geological Society, London, London, United Kingdom
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