Dissolution rates of actinolite and chlorite from a whole-rock experimental study of metabasalt dissolution from 2 ≤ pH ≤ 12 at 25 °C

Author:

Critelli T.,Marini L.,Schott J.,Mavromatis V.,Apollaro C.,Rinder T.,De Rosa R.,Oelkers E.H.

Funder

Regional Operative Program (ROP)

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference78 articles.

1. Investigation of rock-to-water release and fate of major, minor, and trace elements in the metabasalt–serpentinite shallow aquifer of Mt. Reventino (CZ, Italy) by reaction path modelling;Apollaro;Appl. Geochem.,2011

2. The standard thermodynamic properties of vermiculites and prediction of their occurrence during water–rock interaction;Apollaro;Appl. Geochem.,2013

3. Modeling of the impact of dolomite and biotite dissolution on vermiculite composition in a gneissic shallow aquifer of the Sila Massif (Calabria, Italy);Apollaro;Appl. Geochem.,2013

4. Appendix: compilation of mineral dissolution rates;Bandstra,2008

5. Amphibole asbestos and other fibrous minerals in the meta-basalt of the Gimigliano-Mount Reventino Unit (Calabria, South-Italy);Bloise;Rend. Online Soc. Geol. Ital.,2012

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