Iron–clay interactions: Detailed study of the mineralogical transformation of claystone with emphasis on the formation of iron-rich T–O phyllosilicates in a step-by-step cooling experiment from 90 °C to 40 °C-Reference-Cited by-同舟云学术

Iron–clay interactions: Detailed study of the mineralogical transformation of claystone with emphasis on the formation of iron-rich T–O phyllosilicates in a step-by-step cooling experiment from 90 °C to 40 °C

Published:2014-11 Issue: Volume:387 Page:1-11
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Pignatelli Isabella,Bourdelle Franck,Bartier Danièle,Mosser-Ruck Régine,Truche Laurent^ORCID,Mugnaioli Enrico,Michau Nicolas

Funder

ANDRA — Agence nationale pour la gestion des déchets radioactifs

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference49 articles.

1. Odinite, a new dioctahedral-trioctahedral Fe3+-rich 1:1 clay mineral;Bailey;Clay Miner.,1988

2. Matrix phyllosilicates and associated minerals in CM2 carbonaceous chondrites;Barber;Geochim. Cosmochim. Acta,1981

3. Modelling iron–clay interactions in deep geological disposal conditions;Bildstein;Phys. Chem. Earth,2006

4. Thermoddem: a geochemical database focused on low temperature water/rock interactions and waste materials;Blanc;Appl. Geochem.,2012

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