Detrital and xenocrystic zircon ages from Neoproterozoic to Palaeozoic arc terranes of Mongolia: Significance for the origin of crustal fragments in the Central Asian Orogenic Belt-Reference-Cited by-同舟云学术

Detrital and xenocrystic zircon ages from Neoproterozoic to Palaeozoic arc terranes of Mongolia: Significance for the origin of crustal fragments in the Central Asian Orogenic Belt

Published:2011-04 Issue:3 Volume:19 Page:751-763
ISSN:1342-937X
Container-title:Gondwana Research
language:en
Short-container-title:Gondwana Research

Author:

Rojas-Agramonte Y.,Kröner A.,Demoux A.,Xia X.,Wang W.,Donskaya T.,Liu D.,Sun M.

Publisher

Elsevier BV

Subject

Geology

Reference144 articles.

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3. Origin of northern Gondwana Cambrian sandstone revealed by detrital zircon SHRIMP dating;Avigad;Geology,2003

4. A new terrane subdivision for Mongolia: implications for the Phanerozoic crustal growth of Central Asia;Badarch;Journal of Asian Earth Sciences,2002

5. Geodynamic map of Paleo-Asian ocean: eastern segment;Berzin;Russian Geology and Geophysics,1994

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