Retrograde evolution of quartz segregations from the Dos Picos shear zone in the Nevado-Filabride Complex (Betic chains, Spain). Evidence from fluid inclusions and quartz c-axis fabrics

  1. González-Casado, J.M.
  2. Casquet, C.
  3. Martínez-Martinez, J.M.
  4. Garcia-Dueñas, V.
Aldizkaria:
Geologische Rundschau

ISSN: 0016-7835 1437-3262

Argitalpen urtea: 1995

Alea: 84

Zenbakia: 1

Orrialdeak: 175-186

Mota: Artikulua

DOI: 10.1007/BF00192249 GOOGLE SCHOLAR