Interplay Between Crustal‐Scale Thrusting, High Metamorphic Heating Rates, and the Development of Inverted Thermal‐Metamorphic Gradients: Numerical Models and Examples From the Caledonides of Northern Scotland-Reference-Cited by-同舟云学术

Interplay Between Crustal‐Scale Thrusting, High Metamorphic Heating Rates, and the Development of Inverted Thermal‐Metamorphic Gradients: Numerical Models and Examples From the Caledonides of Northern Scotland

Published:2021-11 Issue:11 Volume:40 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Thigpen J. Ryan¹^ORCID,Ashley Kyle T.²^ORCID,Mako Calvin³^ORCID,Law Richard D.²^ORCID,Spencer Brandon¹^ORCID

Affiliation:

1. Department of Earth and Environmental Sciences University of Kentucky Lexington KY USA

2. Department of Geosciences Virginia Tech Blacksburg VA USA

3. Department of Geosciences University of Massachusetts Amherst MA USA

Funder

National Science Foundation

Office of Fossil Energy

Division of Earth Sciences

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021TC006716

Reference70 articles.

1. Brief thermal pulses during mountain building recorded by Sr diffusion in apatite and multicomponent diffusion in garnet

2. Progressive fold and fabric evolution associated with regional strain gradients: a case study from across a Scandian ductile thrust nappe, Scottish Caledonides

3. Garnet morphology distribution in the northern part of the Moine Supergroup, Scottish Caledonides

4. Prograde evolution of the Scottish Caledonides and tectonic implications

5. Mountain Building: From Earthquakes to Geologic Deformation

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