Person:
Arribas Mocoroa, María Eugenia

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First Name
María Eugenia
Last Name
Arribas Mocoroa
URI
https://hdl.handle.net/20.500.14352/75222
Affiliation
Universidad Complutense de Madrid
Faculty / Institute
Ciencias Geológicas
Department
Mineralogía y Petrología
Area
Petrología y Geoquímica
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Author: Comas Rengifo, María José × Subject: 551.7 ×

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    Estratigrafía
    (Coloquios de paleontología, 1992) Rodríguez García, Sergio; Arribas Mocoroa, María Eugenia; Comas Rengifo, María José; Peña, José Andrés de la; Falces, Santiago; Gegúndez, P.; Martínez Chacón, María Luisa; Moreno-Eiris, Elena; Perejón, Antonio; Sánchez Roldán, José Luis; Sáchez Chico, Fátima
    The stratigraphic succession of Los Santos basin can be divided in three groups: a lower group composed mainly of greywackes and volcanie rocks, a middle carbonate group, and an upper siliciclastie group. SANCHEZ el uf (1988) described four lirbologie units (1-4) in the Jower part of the carbonate 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 tbe carbonate rocks (5-6)and the upper siliciclastic rocks (7), based on six new stratigraphic sections, also in the southern area. Finally, FALCES (1991) briefly deseribed 4w lower siliciclastic unit (0), and characterized the variations of the units 1 to 7 on dic basis of several stratigraphical sections in the northern part of the basin: ihe calcareous Units 1,3,4 and 6 yielded abundant fossils and perniited a precise biostratigraplw, based mainly in foraminifers, corals and brachiopods. Sorne Goniatites, conodonts and algae provided additional data.