Departament de Mineralogia, Petrologia i Geologia Aplicada, Facultat de Ciències de la Terra, Universitat de Barcelona, Martí i
Franquès s/n, 08028 Barcelona, Spain
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Cumulative views and downloads
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Total article views: 1,136 (including HTML, PDF, and XML)
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911
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Views and downloads (calculated since 01 Sep 2023)
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287
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Cumulative views and downloads
(calculated since 09 Feb 2023)
Viewed (geographical distribution)
Total article views: 1,550 (including HTML, PDF, and XML)
Thereof 1,487 with geography defined
and 63 with unknown origin.
Total article views: 1,136 (including HTML, PDF, and XML)
Thereof 1,074 with geography defined
and 62 with unknown origin.
Total article views: 414 (including HTML, PDF, and XML)
Thereof 413 with geography defined
and 1 with unknown origin.
Hydration of rocks is a key process in the Earth’s crust and mantle that is accompanied by changes in physical traits and mechanical behaviour of rocks. This study assesses the influence of stress on hydration reaction kinetics and mechanics in experiments on anhydrite. We show that hydration occurs readily under stress and results in localized hydration along fractures and mechanic weakening. New gypsum growth is selective and depends on the stress field and host anhydrite crystal orientation.
Hydration of rocks is a key process in the Earth’s crust and mantle that is accompanied by...