Articles | Volume 11, issue 4
https://doi.org/10.5194/essd-11-1553-2019
https://doi.org/10.5194/essd-11-1553-2019
Data description paper
 | 
17 Oct 2019
Data description paper |  | 17 Oct 2019

Global whole-rock geochemical database compilation

Matthew Gard, Derrick Hasterok, and Jacqueline A. Halpin

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Cited articles

Barette, F., Poppe, S., Smets, B., Benbakkar, M., and Kervyn, M.: Spatial variation of volcanic rock geochemistry in the Virunga Volcanic Province: Statistical analysis of an integrated database, J. Afr. Earth Sci., 134, 888–903, https://doi.org/10.1016/j.jafrearsci.2016.09.018, 2016. a
Barette, F., Poppe, S., Smets, B., Benbakkar, M., and Kervyn, M.: Spatial variation of volcanic rock geochemistry in the Virunga Volcanic Province: Statistical analysis of an integrated database, J. Afr. Earth Sci., 134, 888–903, https://doi.org/10.1016/j.jafrearsci.2016.09.018, 2017. a
Behn, M. and Kelemen, P. B.: Relationship between seismic P-wave velocity and the composition of anhydrous igneous and meta-igneous rocks, Geochem. Geophys. Geosyst., 4, 1041, https://doi.org/10.1029/2002GC000393, 2003. a, b, c
Buggle, B., Glaser, B., Hambach, U., Gerasimenko, N., and Marković, S.: An evaluation of geochemical weathering indices in loess–paleosol studies, Quatern. Int., 240, 12–21, https://doi.org/10.1016/j.quaint.2010.07.019, 2011. a
Carbotte, S. M., Marjanović, M., Carton, H., Mutter, J. C., Canales, J. P., Nedimović, M. R., Han, S., and Perfit, M. R.: Fine-scale segmentation of the crustal magma reservoir beneath the East Pacific Rise, Nat. Geosci., 6, 866–870, https://doi.org/10.1038/ngeo1933, 2013. a
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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.