Study of Iron-Bearing Dolomite Dissolution at Various Temperatures: Evidence for the Formation of Secondary Nanocrystalline Iron-Rich Phases on the Dolomite Surface - Archive ouverte HAL Accéder directement au contenu
Article Dans Une Revue ACS Earth and Space Chemistry Année : 2017

Study of Iron-Bearing Dolomite Dissolution at Various Temperatures: Evidence for the Formation of Secondary Nanocrystalline Iron-Rich Phases on the Dolomite Surface

Paul Mack
  • Fonction : Auteur

Domaines

Matériaux

Dates et versions

hal-01626209 , version 1 (30-10-2017)

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Citer

Mathieu Debure, Pascal Andreazza, Aurélien Canizarès, Sylvain Grangeon, Catherine Lerouge, et al.. Study of Iron-Bearing Dolomite Dissolution at Various Temperatures: Evidence for the Formation of Secondary Nanocrystalline Iron-Rich Phases on the Dolomite Surface. ACS Earth and Space Chemistry, 2017, 1 (7), pp.442 - 454. ⟨10.1021/acsearthspacechem.7b00073⟩. ⟨hal-01626209⟩
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