Rift‐Related Low‐Pressure–High‐Temperature Granulite Facies Metamorphism Generates Widespread Peraluminous Crustal Melts: Evidence From the Early Jurassic Mexican Crust

Rift‐Related Low‐Pressure–High‐Temperature Granulite Facies Metamorphism Generates Widespread Peraluminous Crustal Melts: Evidence From the Early Jurassic Mexican Crust

Abstract High heat fluxes occurring in rift settings are expected to generate partially melted low‐pressure–high‐temperature granulites (LP–HTG). Therefore, studying these rocks can offer valuable insights into crustal reworking during extension. However, our interpretations are limited by the rarit...

Full description

Saved in:
Bibliographic Details
Main Authors: Anthony Ramírez‐Salazar, Mattia Parolari, Arturo Gómez‐Tuena, Fernando Ortega‐Gutiérrez, Mariano Elías‐Herrera
Format: Article
Language:English
Published: Wiley 2025-05-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
rift‐related low‐pressure granulite
crustal reworking
partial melting
hydrate‐breakdown melting
thermodynamic modeling
Pangea breakup
Online Access:https://doi.org/10.1029/2024GC012019
Tags: Add Tag
No Tags, Be the first to tag this record!

Internet

https://doi.org/10.1029/2024GC012019

Similar Items