The configuration of Greater Gondwana—Evidence from LA ICPMS, U–Pb geochronology of detrital zircons from the Palaeozoic and Mesozoic of Southeast Asia and China

Author:

Burrett Clive,Khin Zaw ,Meffre Sebastien,Lai Chun Kit,Khositanont Somboon,Chaodumrong Pol,Udchachon Mongkol,Ekins Samuel,Halpin Jacqueline

Funder

Australian Research Council (ARC)

University of Tasmania (CODES and the School of Earth Science)

Australian Mineral Industry Research Association (AMIRA)

Oxiana Pty Ltd

Publisher

Elsevier BV

Subject

Geology

Reference178 articles.

1. Ordovician conodonts from the Satun area, southern peninsular Thailand;Agematsu;Journal of Paleontology,2007

2. Biostratigraphy and paleobiogeography of Middle and Late Ordovician conodonts from the Langkawi Islands, northern peninsular Malaysia;Agematsu;Journal of Paleontology,2008

3. Detrital zircon U–Pb ages along the Yarlung Tsangpo suture zone, Tibet: implications for oblique convergence and collision between India and Asia;Aitchison;Gondwana Research,2011

4. Akerman, T., 1986. The Geology of the Lower Palaeozoic Tarutao Formation, Tarutao Island, Southern Thailand. Unpublished Honours thesis, University of Tasmania. 84 pp.

5. Palaeomagnetic re-investigation of Early Permian rift basins from the Baoshan Block, SW China: constraints on the site-of-origin of the Gondwana-derived eastern Cimmerian terranes;Ali;Geophysical Journal International,2013

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