K-white mica b cell dimension: a complementary clay mineral tool to decipher a polyphasic basin evolution - Archive ouverte HAL
Communication Dans Un Congrès Année : 2022

K-white mica b cell dimension: a complementary clay mineral tool to decipher a polyphasic basin evolution

Résumé

Since the pioneer work of Sassi (1972) on the K-white mica b cell dimension BCD), the method has been used to characterize the factor pressure in meta-pelitic rocks. This method is used as an estimate of different pressure facies. Studies in the last two decades reached in low-grade metapelitic rocks. Studies in the last two decades have been carried out in different basins and meta-sedimentary rocks with poly-phase evolutions.

Domaines

Minéralogie
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Dates et versions

hal-04295850 , version 1 (23-11-2023)

Identifiants

  • HAL Id : hal-04295850 , version 1

Citer

Sébastien Potel, Rafael Ferreiro Mählmann. K-white mica b cell dimension: a complementary clay mineral tool to decipher a polyphasic basin evolution. AIPEA – XVII INTERNATIONAL CLAY CONFERENCE, THE CLAY SCIENCE SOCIETY (TURKEY); THE CLAY MINERAL SOCIETY (USA); AIPEA, Jul 2022, Istanbul, Turkey. pp.251. ⟨hal-04295850⟩
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