RT Journal Article
T1 Estratigrafía y estructura del área de Los Mansuetos (Cuenca de Teruel). Precisiones para la definición del estratotipo del Turoliense
A1 Calvo Sorando, José Pedro
A1 Alcalá, L.
A1 Alonso Zarza, Ana María
A1 Dam, J. van
A1 Gutíerrez Santolalla, F.
AB Detailed mapping of the Los Mansuetos area, located northeast of the town of Teruel, allows a better lithostratigraphical definition of the Upper Miocene to Pliocene continental sediments exposed in the area. Six main stratigraphic units are distinguished and correlated from E to W of Los Mansuetos. In addition, the complex structure of the area is analyzed: four main fault systems trending NE-SW, NNW-SSE, E-W and NW-SE have been recognized. The NE-SW trending faults and an associated flexure are the youngest structures formed as a result of pervasive dissolution of underlying Triassic evaporite formations cropping out to the north of Los Mansuetos. The other fault systems are probably related to the reactivation of the Teruel and Concud fault systems. The study is relevant in furnishing a more precise geological framework for the stratotype of the Turolian.
PB Sociedad Geológica de España
SN 0213-683X
YR 1998
FD 1998
LK https://hdl.handle.net/20.500.14352/118495
UL https://hdl.handle.net/20.500.14352/118495
LA spa
NO Calvo Sorando, J.P. et al. (1998) «Estratigrafía y estructura del área de Los Mansuetos (Cuenca de Teruel). Precisiones para la definición del estratotipo del Turoliense.», Geogaceta, 25, pp. 55-58.
NO Dirección General de Investigación Científica y Técnica (España)
DS Docta Complutense
RD 13 abr 2025