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Porosity evolution at the brittle-ductile transition in the continental crust: Implications for deep hydro-geothermal circulation

Recently, projects have been proposed to engineer deep geothermal reservoirs in the ductile crust. To examine their feasibility, we performed high-temperature (up to 1000 °C), high-pressure (130 MPa) triaxial experiments on granite (initially-intact and shock-cooled samples) in which we measured the...

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Detalles Bibliográficos
Autores principales: Violay, M., Heap, M. J., Acosta, M., Madonna, C.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5550508/
https://www.ncbi.nlm.nih.gov/pubmed/28794474
http://dx.doi.org/10.1038/s41598-017-08108-5