Isótopos estables de carbono y oxígeno de los rellenos de calcita (falsa ágata) y su interés paleoambiental

  1. Concepción Jiménez de Cisneros Vencelá 1
  2. José Linares González 1
  3. Emilio Reyes Camacho 1
  4. Juan Antonio Vera Torres 2
  1. 1 E. E. Zaidín. CSIC. Granada
  2. 2 Departamento Estratigrafía-Paleontología. Universidad de Granada
Aldizkaria:
Geogaceta

ISSN: 0213-683X

Argitalpen urtea: 1988

Zenbakia: 4

Orrialdeak: 17-20

Mota: Artikulua

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Beste argitalpen batzuk: Geogaceta

Laburpena

The isotopic composition of modern calcite fills (onyx marble) in fractures and related caves is studied. Carbon and oxygen stable isotopes in this material are similar to the vadose speleothems (stalactites and stalagmites) in modern caves and to ca/careous concre- tions in modern soils. This study can contribute to the recognition of analogous deposits in paleokarsts.

Datuen iturria: Dialnet