The relationship between the proportion of microboudinaged columnar grains and far–field differential stress: A numerical model for analyzing paleodifferential stress
Author:
Affiliation:
1. Graduate School of Science and Technology, Educational Division, Shizuoka University
2. Department of Solid Earth Geochemistry, Japan Agency for Marine–Earth Science and Technology
3. Institute of Geoscience, Shizuoka University
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/112/1/112_160711/_pdf
Reference23 articles.
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3. Collins, W.J. and Van Kranendonk, M.J. (1999) Model for the development of kyanite during partial convective overturn of Archaean Granite–Greenstone terranes: the Pilbara Craton, Australia. Journal of Metamorphic Geology, 17, 145–156.
4. Ferguson, C.C. (1981) A strain reversal method for estimating extension from fragmented rigid inclusions. Tectonophysics, 73, 43–52.
5. Kimura, N., Awaji, H., Okamoto, M., Matsumura, Y. and Masuda, T. (2006) Fracture strength of tourmaline and epidote by three–point bending test: application to microboudin method for estimating absolute magnitude of palaeodifferential stress. Journal of Structural Geology, 28, 1093–1102.
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