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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...
Autores principales: | , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2017
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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 |