The core of Rodinia formed by the juxtaposition of opposed retreating and advancing accretionary orogens-Reference-Cited by-同舟云学术

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The core of Rodinia formed by the juxtaposition of opposed retreating and advancing accretionary orogens

Published:2020-12 Issue: Volume:211 Page:103413
ISSN:0012-8252
Container-title:Earth-Science Reviews
language:en
Short-container-title:Earth-Science Reviews

Author:

Martin E.L.,Spencer C.J.,Collins W.J.,Thomas R.J.,Macey P.H.,Roberts N.M.W.

Funder

Australian Government Research Training Program Scholarship

Curtin Senior Research Fellowship

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences

Reference140 articles.

1. The Australo-Antarctic Columbia to Gondwana transition;Aitken;Gondwana Res.,2016

2. A model for the evolution of strontium and lead isotopes in a dynamic;Armstrong;Earth,1968

3. The crustal evolution of South America from a zircon Hf-isotope perspective;Augustsson;Terra Nova,2016

4. Mesoproterozoic rapakivi granites of the Rondônia Tin Province, southwestern border of the Amazonian craton, Brazil — I. Reconnaissance U–Pb geochronology and regional implications;Bettencourt;Precambr. Res.,1999

5. The Rondonian-San Ignacio Province in the SW Amazonian Craton: an overview;Bettencourt;J. South Am. Earth Sci.,2010

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