Departament de Mineralogia, Petrologia i Geologia Aplicada, Facultat de Ciències de la Terra, Universitat de Barcelona, Martí i
Franquès s/n, 08028 Barcelona, Spain
Viewed
Total article views: 2,714 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,115
503
96
2,714
112
119
141
HTML: 2,115
PDF: 503
XML: 96
Total: 2,714
Supplement: 112
BibTeX: 119
EndNote: 141
Views and downloads (calculated since 09 Feb 2023)
Cumulative views and downloads
(calculated since 09 Feb 2023)
Total article views: 2,300 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,828
394
78
2,300
67
114
135
HTML: 1,828
PDF: 394
XML: 78
Total: 2,300
Supplement: 67
BibTeX: 114
EndNote: 135
Views and downloads (calculated since 01 Sep 2023)
Cumulative views and downloads
(calculated since 01 Sep 2023)
Total article views: 414 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
287
109
18
414
45
5
6
HTML: 287
PDF: 109
XML: 18
Total: 414
Supplement: 45
BibTeX: 5
EndNote: 6
Views and downloads (calculated since 09 Feb 2023)
Cumulative views and downloads
(calculated since 09 Feb 2023)
Viewed (geographical distribution)
Total article views: 2,714 (including HTML, PDF, and XML)
Thereof 2,611 with geography defined
and 103 with unknown origin.
Total article views: 2,300 (including HTML, PDF, and XML)
Thereof 2,198 with geography defined
and 102 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...