TY  - JOUR
AU  - Gutiérrez Marco, Juan Carlos
AU  - Sarmiento Chiesa, Graciela Noemí
AU  - Rábano, Isabel
PY  - 2014
SN  - 2255-1379
UR  - https://hdl.handle.net/20.500.14352/33662
T2  - Revista de la Sociedad Geológica de España
AB  - El olistostroma misisípico del Guadalmellato (Serpukhoviense) contiene, 9 km al noroeste de Adamuz (Córdoba), numerosos cantos y bloques fosilíferos del Paleozoico Inferior, incorporados como debritas en las facies lutíticas de talud y mezclados con...
AB  - The Mississippian (Serpukhovian) Guadalmellato olistrostrome, about 9 km northwest of Adamuz (province of Córdoba), includes abundant pebbles and cobbles bearing Lower Paleozoic fosils.They were deposited as debris-flows into slope facies and mixed...
AB  - assemblages. The clastics were derived from an unknown sourcearea adjacent to the Carboniferous Guadiato Basin. The paleobiogeographic affinities of these assemblages display a clear ‘‘Central-Iberian influx’ only during the Middle and Upper...
AB  - reveals that this domain is not a “southern allochtonous unit” defined as an extension of the Central-Iberian Zone. The tectonostratigraphic context of the Serpukhovian olistostrome of the Guadalmellato valley is similar to that of Devonian to...
LA  - spa
M2  - 27
PB  - Sociedad Geológica de España
KW  - Macizo Ibérico
KW  - Dominio Obejo-Valsequillo
KW  - Cuenca del Guadiato
KW  - Olistostroma del Guadalmellato
KW  - Carbonífero
KW  - Silúrico
KW  - Ordovícico
KW  - Iberian Massif
KW  - Obejo-Valsequillo Domain
KW  - Guadiato Basin
KW  - Guadalmellato olistostrome
KW  - Carboniferous
KW  - Silurian
KW  - Ordovician
TI  - Un olistostroma con cantos y bloques del Paleozoico inferior en la cuenca carbonífera del Guadamellato (Córdoba). Parte II : Bioestratigrafía y afinidades paleogeográficas
T2  - A Carboniferous olistostrome with Lower Paleozoic pebbles and cobbles from the Guadalmellato basin (Córdoba). Part II: Biostratigraphy and paleogeographic affinities
TY  - journal article
VL  - 27
ER  -