V004
A multidisciplinary perspective into crustal evolution: from subduction zones to orogens
A multidisciplinary perspective into crustal evolution: from subduction zones to orogens
Session ID#: 251803
Session Description:
The Earth’s crust evolved in response to various physicochemical changes since its formation. This evolution drives a range of processes operating across different tectonic environments (e.g. subduction zone and orogenic belts) and geological conditions (pressure, temperature, redox etc.). These crustal processes require multidisciplinary examination of the various lithologies to gain a full picture of the diverse geological processes of the planet. This session welcomes multidisciplinary studies that utilize diverse approaches to examine crustal processes in various tectonic settings. We welcome contributions that examine any aspects related to metasomatism, low- to high-grade metamorphism, and crustal melting, including but not limited to fluid-rock interaction, redox, rheology, decarbonation, metamorphism, and related metallogenesis.
Co-Sponsor(s):
- T - Tectonophysics
Index Terms:
3613 Subduction zone processes [MINERALOGY AND PETROLOGY]
3652 Pressure-temperature-time paths [MINERALOGY AND PETROLOGY]
3660 Metamorphic petrology [MINERALOGY AND PETROLOGY]
8108 Continental tectonics: compressional [TECTONOPHYSICS]
Primary Convener: Wentao Cao, SUNY at Fredonia, Fredonia, NY, United States and smulligan@niu.edu
Conveners: David Hernández-Uribe, University of Illinois at Chicago, Chicago, United States, Suzanne R Autrey, Western Illinois University, Geoscience, Macomb, United States, Sean R Mulcahy, Western Washington University, Bellingham, United States and smulligan@niu.edu
Student/Early Career Convener: Thomas Lamont, University of Nevada, Las Vegas, Las Vegas, United States and smulligan@niu.edu
See more of: Volcanology, Geochemistry and Petrology