The río Blanco (Soria, Spain) travertine deposits: age and evolution

Abstract

Electro Spin Resonance and Amino Acid Racemizaton dating of Rio Blanco travertine deposits allowed to place travertine platforms bulidup into 9, 7 and 5 Oxigen Isotope Stages. Through topographical situation relative stratigraphy does ?nt work properly because "Las Chorroneras" barrier-water fall influence in backfilling process and local water tabl

    Similar works