Stable Isotope Evidence for Large-Scale Infiltration of Metamorphic Fluids Generated during Shallow Subduction into the Eastern Peninsular Ranges Mylonite Zone (EPRMZ), Southern California-Reference-Cited by-同舟云学术

Stable Isotope Evidence for Large-Scale Infiltration of Metamorphic Fluids Generated during Shallow Subduction into the Eastern Peninsular Ranges Mylonite Zone (EPRMZ), Southern California

Published:2006-03 Issue:3 Volume:48 Page:209-222
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Holk Gregory J.¹,Taylor Hugh P.²,Gromet L. Peter³

Affiliation:

1. a California State University, Long Beach

2. b California Institute of Technology

3. c Brown University

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.2747/0020-6814.48.3.209

Reference57 articles.

1. U.S. Geological Survey, Open-File Report 80-1154;Anderson J. R.,1980

2. Petrology of a portion of the Eastern Peninsular Ranges mylonite zone, Southern California

3. Field-Based Evidence for Devolatilization in Subduction Zones: Implications for Arc Magmatism

4. An integrated chemical and stable-isotope model of the origin of Midocean Ridge Hot Spring Systems

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