The interaction of migrating grain boundaries with fluid inclusions in rock analogues: the effect of wetting angle and fluid inclusion velocity-Reference-Cited by-同舟云学术

The interaction of migrating grain boundaries with fluid inclusions in rock analogues: the effect of wetting angle and fluid inclusion velocity

Published:2010-11-10 Issue:1 Volume:162 Page:193-208
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Schmatz Joyce,Schenk Oliver,Urai Janos L.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-010-0590-3.pdf

Reference57 articles.

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3. Bakker RJ (1992) On modifications of fluid inclusions in quartz. Re-equilibration experiments and thermodynamic calculations on fluids in natural quartz. Unpublished PhD thesis, Rijksuniversiteit Utrecht, Utrecht, pp 189

4. Bauer P, Palm S, Handy MR (2000) Strain localization and fluid pathways in mylonite: inferences from in situ deformation of a water-bearing quartz analogue (norcamphor). Tectonophysics 320(2):141–165

5. Becker JK, Bons PD, Jessell MW (2008) A new front-tracking method to model anisotropic grain and phase boundary motion in rocks. Comput Geosci 34(3):201–212

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