Microstructures and Phase Transition in Omphacite: Constraints on the P-T Path of Shuanghe Eclogite (Dabie Orogen)
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s12583-019-1279-9.pdf
Reference50 articles.
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3. Binns, R. A., 1967. Barroisite-Bearing Ecologite from Naustdal, Song Og Fjordane, Norway. Journal of Petrology, 8(3): 349–371. https://doi.org/10.1093/petrology/8.3.349
4. Brenker, F. E., Müller, W. F., Brey, G. P., 2003. Variation of Antiphase Domain Size in Omphacite: A Tool to Determine the Temperature-Time History of Eclogites Revisited. American Mineralogist, 88(8/9): 1300–1311. https://doi.org/10.2138/am-2003-8-912
5. Brenker, F. E., Prior, D. J., Müller, W. F., 2002. Cation Ordering in Ompha-cite and Effect on Deformation Mechanism and Lattice Preferred Orientation (LPO). Journal of Structural Geology, 24(12): 1991–2005. https://doi.org/10.1016/s0191-8141(02)00010-x
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