Quartz preferred orientation in naturally deformed mylonitic rocks (Montalto shear zone–Italy): a comparison of results by different techniques, their advantages and limitations
Author:
Funder
NSF
DOE
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://link.springer.com/article/10.1007/s00531-016-1424-y/fulltext.html
Reference90 articles.
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2. Baker DW, Wenk HR, Christie JM (1969) X-ray analysis of preferred orientation in fine-grained quartz aggregates. J Geol 77:143–172
3. Barrett SD (2008) Image SXM. http://www.ImageSXM.org.uk
4. Bestmann M, Kunze K, Matthews A (2000) Evolution of a calcite marble shear zone complex on Thassos Island, Greece: microstructural and textural fabrics and their kinematic significance. J Struct Geol 22:1789–1807
5. Cirrincione R, Ortolano G, Pezzino A, Punturo R (2008) Poly-orogenic multi-stage metamorphic evolution inferred via P–T pseudosections: an example from Aspromonte Massif basement rocks (Southern Calabria, Italy). Lithos 103:466–502
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