Las areniscas de la Formación de Gordexola (Albiense, flanco sur del Anticlinorio de Bilbao, Vizcaya)IICementación y diagénesis.

  1. Zuluaga, M.C.
  2. García Garmilla, F.
  3. Arostegui, J.
Aldizkaria:
Geogaceta

ISSN: 0213-683X

Argitalpen urtea: 1997

Zenbakien izenburua: 22ª Sesión Científica, Bilbao 1997

Zenbakia: 22

Orrialdeak: 219-222

Mota: Artikulua

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Beste argitalpen batzuk: Geogaceta

Laburpena

The sandstones of the Gordexola Formation were studied using petrography, cathodoluminescence, electronic microprobe, SEM, and C and O isotopic relations. A diagenetic sequence was inferred from medium to late stages. The processes that affected sandstones occurred from syntaxial siliceous cements to different carbonates that precipitated and replaced previous felsdpar grains. Temperatures of late diagenesis could oscillate from 40° to 45° C. The very late diagenesis consisted on deformation of both grains and crystals under burial conditions.

Datuen iturria: Dialnet