Post-tilleyite, a dense calcium silicate-carbonate phase

Calcium carbonate is a relevant constituent of the Earth’s crust that is transferred into the deep Earth through the subduction process. Its chemical interaction with calcium-rich silicates at high temperatures give rise to the formation of mixed silicate-carbonate minerals, but the structural behav...

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Veröffentlicht in:Scientific reports 2019-05, Vol.9 (1), p.7898-7898, Article 7898
Hauptverfasser: Santamaria-Perez, David, Ruiz-Fuertes, Javier, Peña-Alvarez, Miriam, Chulia-Jordan, Raquel, Marqueño, Tomas, Zimmer, Dominik, Gutiérrez-Cano, Vanessa, MacLeod, Simon, Gregoryanz, Eugene, Popescu, Catalin, Rodríguez-Hernández, Plácida, Muñoz, Alfonso
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container_title Scientific reports
container_volume 9
creator Santamaria-Perez, David
Ruiz-Fuertes, Javier
Peña-Alvarez, Miriam
Chulia-Jordan, Raquel
Marqueño, Tomas
Zimmer, Dominik
Gutiérrez-Cano, Vanessa
MacLeod, Simon
Gregoryanz, Eugene
Popescu, Catalin
Rodríguez-Hernández, Plácida
Muñoz, Alfonso
description Calcium carbonate is a relevant constituent of the Earth’s crust that is transferred into the deep Earth through the subduction process. Its chemical interaction with calcium-rich silicates at high temperatures give rise to the formation of mixed silicate-carbonate minerals, but the structural behavior of these phases under compression is not known. Here we report the existence of a dense polymorph of Ca 5 (Si 2 O 7 )(CO 3 ) 2 tilleyite above 8 GPa. We have structurally characterized the two phases at high pressures and temperatures, determined their equations of state and analyzed the evolution of the polyhedral units under compression. This has been possible thanks to the agreement between our powder and single-crystal XRD experiments, Raman spectroscopy measurements and ab-initio simulations. The presence of multiple cation sites, with variable volume and coordination number (6–9) and different polyhedral compressibilities, together with the observation of significant amounts of alumina in compositions of some natural tilleyite assemblages, suggests that post-tilleyite structure has the potential to accommodate cations with different sizes and valencies.
doi_str_mv 10.1038/s41598-019-44326-9
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subjects 119/118
140/133
639/301/119
704/2151/330
Aluminum oxide
Calcium carbonate
Carbon
Cations
Compression
High temperature
Humanities and Social Sciences
Minerals
multidisciplinary
Powder
Raman spectroscopy
Science
Science (multidisciplinary)
Silica
Silicates
Spectrum analysis
Structural behavior
title Post-tilleyite, a dense calcium silicate-carbonate phase
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