Metamorphic Evolution and Tectonic Implications of Garnet-Bearing Mica Schist in Sumdo High Pressure Belt from Eastern Lhasa Block, Tibet

The garnet-bearing mica-quartz schist of the Sumdo high pressure metamorphic beltfrom the Lhasa block is mainly composed of garnet, muscovite, albite, quartz and minor chlorite, rutile and sphene.

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Bibliographic Details
Published inActa geologica Sinica (Beijing) Vol. 89; no. s2; pp. 3 - 4
Main Authors CHEN, Mei, YANG, Jingsui, ZHANG, Cong, TIAN, Zuolin, HUANG, Jie, YU, Huanglu, DONG, Tianci
Format Journal Article
LanguageEnglish
Published Richmond Blackwell Publishing Ltd 01.12.2015
Wiley Subscription Services, Inc
EditionEnglish ed.
Subjects
High pressure
China, People's Rep., Xizang
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Summary:The garnet-bearing mica-quartz schist of the Sumdo high pressure metamorphic beltfrom the Lhasa block is mainly composed of garnet, muscovite, albite, quartz and minor chlorite, rutile and sphene.
Bibliography:The garnet-bearing mica-quartz schist of the Sumdo high pressure metamorphic beltfrom the Lhasa block is mainly composed of garnet, muscovite, albite, quartz and minor chlorite, rutile and sphene.
11-2001/P
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ark:/67375/WNG-DJWVTQDP-2
ArticleID:ACGS12308_3
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:1000-9515
1755-6724
DOI:10.1111/1755-6724.12308_3