RT Journal Article
T1 Reconocimiento de acumulaciones travertínicas fósiles en la Fm. Aguilar (Kimmeridgiense-Berriasiense de Palencia y Burgos): implicaciones paleoecológicas y paleohidrológicas
T1 Recognition of fossil travertine accumulations in the Aguilar Fm. (Kimmeridgian-Berriasian of Palencia and Burgos): palaeoecological and palaeohidrological implications
A1 Hernández, José María
A1 Diéguez, C.
A1 Pujalte, Victoriano
A1 Robles, Sergio
A1 Wright, V. P.
AB Fossil travertine deposits have been recognized in the Aguilar Fm., which are intercalated vyithin the typical lacüstrine/palustrine limestones of this unit. Microscopically, they are characterised by numerous plant, remains and microscopically by abundant features atributáble to microbial, activity. The travertine accumulation occurred next to an important fault line that was contemporaneously active. 'Because of that; they are thought to record former hot-springs within a discharge-type water inflow system
PB Sociedad Geológica de España
YR 1997
FD 1997
LK http://hdl.handle.net/10272/10329
UL http://hdl.handle.net/10272/10329
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026