Supplemental Information: Magmatic water variation in Neo-Tethys: controlled by convergence rate and slab geometry

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Auteurs principaux: Wu, Shaochen, Wang, Rui, Zhong, Xinyi
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Publié: Zenodo 2025
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author Wu, Shaochen
Wang, Rui
Zhong, Xinyi
author_facet Wu, Shaochen
Wang, Rui
Zhong, Xinyi
contents <p>Wholerock geochemistry data.xlsx: Compiled whole-rock geochemical database of the Gangdese belt.<br>Trace element partition coefficient.xlsx: Partition coefficients of four minerals downloaded from EarthRef.org.<br>Main element concentration.xlsx: Main element concentrations of all minerals chosen in four mineral groups.<br>Viscous flow law parameters.xlsx: Rheological parameters used in numerical modeling.<br>Material properties.xlsx: Material properties used in numerical modeling.<br>Fractional crystallization model results.xlsx: Results of fractional crystallization modeling with a moving window of 30-Ma and a step of 5-Ma on the data of the Gangdese belt. Three sheets of P, D, and C0 are parameters in the fractional crystallization model. See detailed explanations in the Methods section.<br>Fractional crystallization model bootstraps.xlsx: Results of 1000 bootstraps for the modeling in Fractional crystallization model results.xlsx. Each lines represents a bootstrap result. Columns are index from 0 to 37 representing the time intervals used in Fractional crystallization model results.xlsx. Values in cell are only the parameter of proportion (the sum of each mineral groups).</p>
format Recurso digital
id zenodo_https___doi_org_10_5281_zenodo_16751353
institution Zenodo
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publishDate 2025
publisher Zenodo
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spellingShingle Supplemental Information: Magmatic water variation in Neo-Tethys: controlled by convergence rate and slab geometry
Wu, Shaochen
Wang, Rui
Zhong, Xinyi
<p>Wholerock geochemistry data.xlsx: Compiled whole-rock geochemical database of the Gangdese belt.<br>Trace element partition coefficient.xlsx: Partition coefficients of four minerals downloaded from EarthRef.org.<br>Main element concentration.xlsx: Main element concentrations of all minerals chosen in four mineral groups.<br>Viscous flow law parameters.xlsx: Rheological parameters used in numerical modeling.<br>Material properties.xlsx: Material properties used in numerical modeling.<br>Fractional crystallization model results.xlsx: Results of fractional crystallization modeling with a moving window of 30-Ma and a step of 5-Ma on the data of the Gangdese belt. Three sheets of P, D, and C0 are parameters in the fractional crystallization model. See detailed explanations in the Methods section.<br>Fractional crystallization model bootstraps.xlsx: Results of 1000 bootstraps for the modeling in Fractional crystallization model results.xlsx. Each lines represents a bootstrap result. Columns are index from 0 to 37 representing the time intervals used in Fractional crystallization model results.xlsx. Values in cell are only the parameter of proportion (the sum of each mineral groups).</p>
title Supplemental Information: Magmatic water variation in Neo-Tethys: controlled by convergence rate and slab geometry
url https://doi.org/10.5281/zenodo.16751353