Kinematic, Deformational, and Thermochronologic Conditions Along the Gossan Lead and Fries Shear Zones: Constraining the Western‐Eastern Blue Ridge Boundary in Northwestern North Carolina-Reference-Cited by-同舟云学术

Kinematic, Deformational, and Thermochronologic Conditions Along the Gossan Lead and Fries Shear Zones: Constraining the Western‐Eastern Blue Ridge Boundary in Northwestern North Carolina

Published:2018-10 Issue:10 Volume:37 Page:3500-3523
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Levine J. S. F.¹^ORCID,Merschat A. J.²^ORCID,McAleer R. J.²^ORCID,Casale G.¹,Quillan K. R.³,Fraser K. I.¹,BeDell T. G.¹^ORCID

Affiliation:

1. Department of Geological and Environmental Sciences Appalachian State University Boone NC USA

2. U.S. Geological Survey Reston VA USA

3. Materials Testing & Consulting, Inc. Bellingham WA USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2017TC004879

Reference118 articles.

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2. The Ashe Metamorphic Suite, Northwest North Carolina; metamorphism and observations on geologic history

3. Granulites at Winding Stair Gap, North Carolina: The thermal axis of Paleozoic metamorphism in the southern Appalachians

4. Adams M.G.(2000).The nature of the eastern‐western Blue Ridge contact across the Grandfather Mountain window: Geological Society of America Abstracts with Programs 32 1.

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