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Petrological and Metamorphic Evolution Study of the Staurolite‐bearing Garnet Amphibolite in the Nyingchi Complex of the Lhasa Block

Petrological and Metamorphic Evolution Study of the Staurolite‐bearing Garnet Amphibolite in the... Dec. 2015 HUANG Jie, ZHANG Cong , YANG Jingsui,CHEN Mei and SHENG Tingting, 2015. Petrological and Metamorphic Evolution Study of the Staurolite-bearing Garnet Amphibolite in the Nyingchi Complex of the Lhasa Block. Acta Geologica Sinica (English Edition), 89(supp. 2): 28-29. Petrological and Metamorphic Evolution Study of the Staurolite-bearing Garnet Amphibolite in the Nyingchi Complex of the Lhasa Block HUANG Jie1,2, ZHANG Cong1*, YANG Jingsui1,CHEN Mei1,2 and SHENG Tingting3 1 State Key Laboratory for Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing100037, China; 2 School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China; 3 School of Earth and Space Sciences, Peking University, Beijing 100871, China 1 Introduction Metamorphosed mafic rocks in orogenic belts usually involve high-variance assemblages which are stable very large regions of pressure (P)–temperature (T) and compositional (X) space. In particular, amphibolite facies mafic rocks typically contain similar assemblages: hornblende, plagioclase and epidote, This common assemblage is not enough to calculate the temperature and pressure. However, the existence of Al-rich minerals makes it possible to do the P-T study. 2 P-T Evolution of Staurolite-bearing Garnet Amphibolites The newly-found, staurolite-bearing garnet amphibolites in the Nyingchi complex of the http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta Geologica Sinica (English Edition) Wiley

Petrological and Metamorphic Evolution Study of the Staurolite‐bearing Garnet Amphibolite in the Nyingchi Complex of the Lhasa Block

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Publisher
Wiley
Copyright
© 2015 Geological Society of China
ISSN
1000-9515
eISSN
1755-6724
DOI
10.1111/1755-6724.12308_20
Publisher site
See Article on Publisher Site

Abstract

Dec. 2015 HUANG Jie, ZHANG Cong , YANG Jingsui,CHEN Mei and SHENG Tingting, 2015. Petrological and Metamorphic Evolution Study of the Staurolite-bearing Garnet Amphibolite in the Nyingchi Complex of the Lhasa Block. Acta Geologica Sinica (English Edition), 89(supp. 2): 28-29. Petrological and Metamorphic Evolution Study of the Staurolite-bearing Garnet Amphibolite in the Nyingchi Complex of the Lhasa Block HUANG Jie1,2, ZHANG Cong1*, YANG Jingsui1,CHEN Mei1,2 and SHENG Tingting3 1 State Key Laboratory for Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing100037, China; 2 School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China; 3 School of Earth and Space Sciences, Peking University, Beijing 100871, China 1 Introduction Metamorphosed mafic rocks in orogenic belts usually involve high-variance assemblages which are stable very large regions of pressure (P)–temperature (T) and compositional (X) space. In particular, amphibolite facies mafic rocks typically contain similar assemblages: hornblende, plagioclase and epidote, This common assemblage is not enough to calculate the temperature and pressure. However, the existence of Al-rich minerals makes it possible to do the P-T study. 2 P-T Evolution of Staurolite-bearing Garnet Amphibolites The newly-found, staurolite-bearing garnet amphibolites in the Nyingchi complex of the

Journal

Acta Geologica Sinica (English Edition)Wiley

Published: Dec 1, 2015

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