Fracturing, fluid flow and shear zone development: Relationships between chemical and mechanical processes in Proterozoic mafic dykes from southwestern Montana, USA-Reference-Cited by-同舟云学术

Fracturing, fluid flow and shear zone development: Relationships between chemical and mechanical processes in Proterozoic mafic dykes from southwestern Montana, USA

Published:2017-12-06 Issue:2 Volume:36 Page:195-223
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J Metamorph Geol

Author:

Condit Cailey B.¹^ORCID,Mahan Kevin H.²

Affiliation:

1. Department of Earth, Environmental and Planetary Sciences Rice University Houston TX USA

2. Department of Geological Sciences University of Colorado Boulder Boulder CO USA

Funder

National Science Foundation

U.S. Geological Survey

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/jmg.12289

Reference83 articles.

1. Subduction interface processes recorded by eclogite-facies shear zones (Monviso, W. Alps)

2. Diffusion-accommodated flow and superplasticity

3. Quartz shielding of sub-10μm zircons from radiation damage-enhanced Pb loss: An example from a metamorphosed mafic dike, northwestern Wyoming craton

4. Eclogitization of lower crustal granulites by fluid migration through shear zones

5. Shear deformation and eclogite formation within granulite-facies anorthosites of the Bergen Arcs, western Norway

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