Articles | Volume 11, issue 4
https://doi.org/10.5194/essd-11-1553-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/essd-11-1553-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Global whole-rock geochemical database compilation
Matthew Gard
CORRESPONDING AUTHOR
Department of Earth Sciences, University of Adelaide, North
Terrace, SA, 5005, Australia
Derrick Hasterok
Department of Earth Sciences, University of Adelaide, North
Terrace, SA, 5005, Australia
Mawson Centre for Geoscience (MCG), University of Adelaide, North Terrace, SA, 5005, Australia
Jacqueline A. Halpin
Institute for Marine and Antarctic Studies (IMAS), University of Tasmania, Hobart, TAS, 7001, Australia
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50 citations as recorded by crossref.
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- Geological evidence for high H2 production from komatiites in the Archaean R. Tamblyn & J. Hermann 10.1038/s41561-023-01316-x
- Plate tectonics: What, where, why, and when? R. Palin & M. Santosh 10.1016/j.gr.2020.11.001
- Four billion years of secular compositional change in granitoids K. Condie et al. 10.1016/j.chemgeo.2023.121868
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- Mantle heating at ca. 2 Ga by continental insulation: Evidence from granites and eclogites R. Tamblyn et al. 10.1130/G49288.1
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Latest update: 05 Dec 2024
Short summary
We compiled a database of more than 1 million chemical analyses of igneous, sedimentary and metamorphic rocks, derived from existing databases, governmental data and academic studies. Our database enhances temporal distributions, simplifies the structure, and adds geochemical indices, naming schema, and estimates of physical properties such as density. This database provides a source for the rapid production of crustal models and chemical evolution throughout 4 billion years of geologic history.
We compiled a database of more than 1 million chemical analyses of igneous, sedimentary and...
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