ptx.ess ucla.edu

UCLA PTX Lab -- experimental petrology at the University of California, Los Angeles

Recent results in our lab suggest a simple mechanism for the dissolution of common, congruently-soluble rock-forming minerals in saline fluids at deep crustal conditions. Dissolution texture of a corundum crystal. The 1950 quartz solubility plot by George Kennedy that started it all. Kennedy GC 1950b A portion of the system silica-water. Economic Geology, 45, 629-653. PTX Experimental Petrology Lab, Department of Earth and Space Sciences.

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LINKS TO DOMAIN

UCLA - Earth, Planetary, and Space Sciences

Earth, Planetary, and Space Sciences. Earth, Planetary, and Space Sciences. Department of Earth, Planetary, and Space Sciences. The largest on the West Coast. UCLA Institute for Planets and Exoplanets. Alumni gifts enhance undergraduate education. Climate and Carbon Cycle Group.

EPIC - Experimental Petrology and Igneous processes Center

Enter in the School of Earth and Space Exploration. We do this through studying volcanoes and their magma source regions, conducting high pressure and temperature experiments to simulate magma formation in the lab, and computational modeling of magmatic processes.

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HTML TITLE

UCLA PTX Lab -- experimental petrology at the University of California, Los Angeles

DESCRIPTION

Recent results in our lab suggest a simple mechanism for the dissolution of common, congruently-soluble rock-forming minerals in saline fluids at deep crustal conditions. Dissolution texture of a corundum crystal. The 1950 quartz solubility plot by George Kennedy that started it all. Kennedy GC 1950b A portion of the system silica-water. Economic Geology, 45, 629-653. PTX Experimental Petrology Lab, Department of Earth and Space Sciences.

PARSED CONTENT

The website ptx.ess.ucla.edu states the following, "Recent results in our lab suggest a simple mechanism for the dissolution of common, congruently-soluble rock-forming minerals in saline fluids at deep crustal conditions." We analyzed that the webpage said " Dissolution texture of a corundum crystal." It also stated " The 1950 quartz solubility plot by George Kennedy that started it all. Kennedy GC 1950b A portion of the system silica-water. Economic Geology, 45, 629-653. PTX Experimental Petrology Lab, Department of Earth and Space Sciences."

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