Late Eocene-Oligocene granulite facies garnet-sillimanite migmatites from the Mogok Metamorphic belt, Myanmar, and implications for timing of slip along the Sagaing Fault-Reference-Cited by-同舟云学术

Late Eocene-Oligocene granulite facies garnet-sillimanite migmatites from the Mogok Metamorphic belt, Myanmar, and implications for timing of slip along the Sagaing Fault

Published:2021-04 Issue: Volume:386-387 Page:106027
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Lamont T.N.,Searle M.P.,Hacker B.R.,Htun Kyi,Htun Kyaw Min,Morley C.K.,Waters D.J.,White R.W.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference92 articles.

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4. Tectonics of the western margin of the Shan plateau (Central Myanmar): implication for the India–Indochina oblique convergence since the Oligocene;Bertrand;J. Asian Earth Sci.,2003

5. Diachronous cooling along the Mogok Metamorphic Belt (Shan Scarp, Myanmar): the trace of the northward migration of the Indian syntaxis;Bertrand;J. Asian Earth Sci.,2001

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