%0 Journal Article
%A Rodríguez García, Sergio
%A Arribas Mocoroa, María Eugenia
%A Comas Rengifo, María José
%A Peña, José Andrés de la
%A Falces, Santiago
%A Gegúndez, P.
%A Martínez Chacón, María Luisa
%A Moreno-Eiris, Elena
%A Perejón, Antonio
%A Sánchez Roldán, José Luis
%A Sáchez Chico, Fátima
%T Estratigrafía
%D 1992
%@ 1132-1660
%U https://hdl.handle.net/20.500.14352/57746
%X 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.
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