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  1. Yadanabon University
  2. Department of Geology

"Metamorphic Facies and Retrograde Metamorphism of the Myogyi Area, Ywangan Township, Southern Shan State"

https://meral.edu.mm/records/8404
https://meral.edu.mm/records/8404
a55d2be8-3858-4656-915d-826bed37a269
feb276db-45ff-43f0-ba1a-26082d0d3c22
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Aye Aye Aye Mar.pdf (1.6 MB)
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Journal article
Upload type
Publication
Title
Title "Metamorphic Facies and Retrograde Metamorphism of the Myogyi Area, Ywangan Township, Southern Shan State"
Language en
Authors
Aye Aye Mar
Naing Lin
Marlar Aye Shwe
Description
"The regionally metamorphosed rocks that are occurred in the study area have undergone
deformation during Charnian orogenic event resulting that have been eroded to expose
the metamorphic rocks. The major rock units in the study area are mainly composed of
metasedimentary rocks of metapelite (Slate, Phyllite and Schist) and metapsammite
(Quartzite and Metagreywacke). The texture of the rocks changes from Slates and Phyllites
in the Chlorite zone to Mica - Schists in the Biotite zones, to Garnet -Mica Schists in the
Garnet zone. The metamorphic facies series of regional metamorphism are characterized
by the presence of garnet and chloritoid in the intermediate grade mineral assemblages
indicating that the conditions of metamorphism in Barrovian Facies Series of
metamorphic rocks. The greenschist facies for Phyllite and Mica - Schist and the epidote
amphibolite facies for Garnet - Mica schist occurred in the study area. In the study area,
the garnet porphyroblasts are often rimmed by small amounts of chlorite and quartz,
indicating that limited quantities of water were available for the reverse of the reaction
given above to proceed during cooling. The chlorite rims on the garnet porphyroblasts
indicate the retrograte metamorphism."
Keywords
Charnian orogenic event, metapelite, metapsammite, chloritoid, metapelite, metapsammite, chloritoid
Journal articles
2022
Yadanabon University Research Journal
165-174
Vol.12, No.2
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