RT Journal Article
T1 Estratigrafía
A1 Rodríguez, Sergio
A1 Arribas Mocoroa, María Eugenia
A1 Comas Rengifo, María José
A1 Peña, José Andrés de la
A1 Falces, Santiago
A1 Gegúndez, P.
A1 Martínez Chacón, María Luisa
A1 Moreno-Eiris, Elena
A1 Perejón, Antonio
A1 Sánchez, J.L.
A1 Sáchez Chico, Fátima
AB The stratigraphic succession of Los Santos basin can be divided in three groups: alower group composed mainly of greywackes and volcanie rocks, a middle carbonategroup, and an upper siliciclastie group.SANCHEZ el uf (1988) described four lirbologie units (1-4) in the Jower part of thecarbonate sediments based on five stratigraphic seetions iii tbe southern part of the basin.RODRÍGUEZ et al., in press) defined duce units, including the upper part of tbecarbonate rocks (5-6)and the upper siliciclastic rocks (7), based on six new stratigraphicsections, also in the southern area. Finally, FALCES (1991) briefly deseribed 4w lowersiliciclastic unit (0), and characterized the variations of the units 1 to 7 on dic basis ofseveral stratigraphical sections in the northern part of the basin:ihe calcareous Units 1,3,4 and 6 yielded abundant fossils and perniited a precisebiostratigraplw, based mainly in foraminifers, corals and brachiopods. Sorne Goniatites,conodonts and algae provided additional data.
PB Universidad Complutense de Madrid, Servicio de Publicaciones
SN 1132-1660
YR 1992
FD 1992
LK https://hdl.handle.net/20.500.14352/57746
UL https://hdl.handle.net/20.500.14352/57746
LA spa
DS Docta Complutense
RD 4 may 2024