Sapphirine-Bearing Pelitic Granulite from Ailaoshan Orogen, West Yunnan, China: Metamorphic Conditions and Tectonic Setting
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://link.springer.com/content/pdf/10.1007/s12583-019-0893-x.pdf
Reference83 articles.
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2. Anderson, J. R., Payne, J. L., Kelsey, D. E., et al., 2012. High-Pressure Granulites at the Dawn of the Proterozoic. Geology, 40(5): 431–434. https://doi.org/10.1130/g32854.1
3. Bertrand, P., Ellis, D. J., Green, D. H., 1991. The Stability of Sapphirine-Quartz and Hypersthene-Sillimanite-Quartz Assemblages: An Experimental Investigation in the System FeO-MgO-Al2O3-SiO2 under H2O and CO2 Conditions. Contributions to Mineralogy and Petrology, 108(1/2): 55–71. https://doi.org/10.1007/bf00307326
4. Brown, M., 2007. Metamorphic Conditions in Orogenic Belts: A Record of Secular Change. International Geology Review, 49(3): 193–234. https://doi.org/10.2747/0020-6814.49.3.193
5. Burchfiel, B. C., Wang, E., 2003. Northwest-Trending, Middle Cenozoic, Left-Lateral Faults in Southern Yunnan, China, and Their Tectonic Significance. Journal of Structural Geology, 25(5): 781–792. https://doi.org/10.1016/s0191-8141(02)00065-2
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