2023
DOI: 10.22541/essoar.169111678.88422505/v1
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Is the inverted field gradient in the Catalina Schist Terrane primary or constructional?

Abstract: New geothermometry shows that high-pressure rocks on Catalina define an inverted metamorphic temperature zonation • The zonation is disrupted, and the present structure does not represent an original inverted thermal gradient • The zonation formed by progressive underplating in a cooling subduction zone following a high-T metamorphic event

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“…Please cite these data as J. Platt & Schmidt, 2023. Laser Raman analysis of carbonaceous material, Catalina subduction complex, California, Version 1.0.…”
Section: Data Availability Statementmentioning
confidence: 99%
“…Please cite these data as J. Platt & Schmidt, 2023. Laser Raman analysis of carbonaceous material, Catalina subduction complex, California, Version 1.0.…”
Section: Data Availability Statementmentioning
confidence: 99%