Research Article|
December 01, 2020
New Ti-in-quartz diffusivities reconcile natural Ti zoning with time scales and temperatures of upper crustal magma reservoirs: COMMENT Open Access
Guilherme A.R. Gualda;
Guilherme A.R. Gualda
1
Earth & Environmental Sciences, Vanderbilt University, PMB 351805, 2301 Vanderbilt Place, Nashville, Tennessee 37235-1805, USA
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Ayla S. Pamukçu
Ayla S. Pamukçu
2
Geological Sciences, Stanford University, 450 Jane Stanford Way, Building 320, Room 118 Stanford, California 94305-2115, USA
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Guilherme A.R. Gualda
1
Earth & Environmental Sciences, Vanderbilt University, PMB 351805, 2301 Vanderbilt Place, Nashville, Tennessee 37235-1805, USA
Ayla S. Pamukçu
2
Geological Sciences, Stanford University, 450 Jane Stanford Way, Building 320, Room 118 Stanford, California 94305-2115, USA
Publisher: Geological Society of America
First Online:
24 Nov 2020
Online ISSN: 1943-2682
Print ISSN: 0091-7613
© 2020 Geological Society of America
Geology (2020) 48 (12): e513.
Article history
First Online:
24 Nov 2020
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CitationGuilherme A.R. Gualda, Ayla S. Pamukçu; New Ti-in-quartz diffusivities reconcile natural Ti zoning with time scales and temperatures of upper crustal magma reservoirs: COMMENT. Geology 2020;; 48 (12): e513. doi: https://doi.org/10.1130/G48242C.1
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