Etd

 

Pressure Temperature Deformation History Of The Ollo De Sapo Antiform, Variscan Orogen, Northwest Spain. Open Access Deposited

Downloadable Content

Download PDF
Download Adobe Acrobat Reader
Date Uploaded: 03/26/2018
Date Modified: 03/26/2018

Metamorphism in the Ollo de Sapo Antiform, part of the Variscan Orogen in NW Spain, was controlled by local, complex interactions of deformation, granitoid intrusions, and regional low pressure metamorphic (LPM) gradient. Detailed analysis of mineral parageneses, in conjunction with geothermobarometry and one-dimensional thermal modeling, have been used to constrain pressure-temperature-deformation (P-T-D) paths for rocks in the antiform.

Creator
License
Subject
Submitter
College
Degree Program
Degree
  • Ph.D.
Degree Date
Advisor
  • Chair: Craig W. Dietsch.
Publisher
Language

Relationships

Items

Permanent link to this page: https://scholar.uc.edu/show/k0698755v