Browsing by Author "Badarch G."
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Browsing by Author "Badarch G."
Now showing items 1-9 of 9
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Badarch G.; Dickson Cunningham W.; Windley B.F. (2002)We 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. Forty-four terranes are ...
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Kröner A.; Windley B.F.; Badarch G.; Tomurtogoo O.; Hegner E.; Jahn B.M.; Gruschka S.; Khain E.V.; Demoux A.; Wingate M.T.D. (2007)The Central Asian Orogenic Belt is one of the largest accretionary terrains on Earth and records a ca. 800 Ma history of arc and microcontinent accretion, from south to north, during evolution and closure of the southwest ...
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Cunningham D.; Dijkstra A.; Howard J.; Quarles A.; Badarch G. (2003)The Mongolian Altai is a Late Cenozoic intraplate strike-slip deformation belt which formed as a distant strain response to the Indo-Eurasian collision over 2000 km to the south. We report results from 5 weeks of detailed ...
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Cunningham D.; Davies S.; Badarch G. (2003)The Sutai Range is a structural and topographic culmination at the southeastern end of the Mongolian Altai and a world-class example of an actively forming restraining bend. The range occurs at a major stepover zone along ...
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Webb L.E.; Graham S.A.; Johnson C.L.; Badarch G.; Hendrix M.S. (1999)Mylonitic rocks associated with the south-dipping detachment fault of the Yagan Onch Hayrhan metamorphic core complex in southernmost Mongolia indicate subhorizontal south-southeast directed extension in the Early Cretaceous; ...
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Xiao W.; Sun S.; Li J.; Qin K.; Wang Z.; Windley B.F.; Badarch G. (2004)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 ...
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Ruzhentsev S.V.; Badarch G. (1989)The Paleozoic fold belt of southern Mongolia includes two systems, the Variscan (South Mongolian) and the Indosinian (Inner Mongolian or East Gobi). The first arose in the Early Carboniferous in the area of an old ocean ...
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Jahn B.-M.; Capdevila R.; Vernon A.; Liu D.; Badarch G. (2004)The Central Asian Orogenic Belt (CAOB) is renowned for massive generation of juvenile crust in the Phanerozoic. Mongolia is the heartland of the CAOB and it has been subject to numerous investigations, particularly in ...
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Windley B.F.; Cunningham W.D.; Buchan A.C.; Badarch G.; Tomurtogoo O.; Kröner A.; Salnikova E.B. (2001)
Now showing items 1-9 of 9