High pressure and HP-HT behaviour of lizardite and chlorite

DOI

Layered minerals such as lizardite and chlorite are believed to be possible water-carrier in the deep Earth crust. However, the high-pressure behaviour of layered minerals is still poorly constrained. This is due to several factors, including the layered nature of these minerals that often result in the acquisition of low-quality single crystal data. Because of that, we selected several single crystal of both specimens, collected from renowned outcrops. The main target of this proposal is to investigate the structure evolution and the high-pressure behaviour of lizardite and chlorite in order to better constrain their PT stability range.

Identifier
DOI https://doi.org/10.15151/ESRF-ES-1020368256
Metadata Access https://icatplus.esrf.fr/oaipmh/request?verb=GetRecord&metadataPrefix=oai_datacite&identifier=oai:icatplus.esrf.fr:inv/1020368256
Provenance
Creator Michael HANFLAND; Tomasz POREBA; Gaston GARBARINO ORCID logo; Benedetta CHRAPPAN SOLDAVINI; Davide COMBONI ORCID logo; Marco MERLINI
Publisher ESRF (European Synchrotron Radiation Facility)
Publication Year 2025
Rights CC-BY-4.0; https://creativecommons.org/licenses/by/4.0
OpenAccess true
Representation
Resource Type Data from large facility measurement; Collection
Discipline Particles, Nuclei and Fields