TY  - JOUR
AU  - Moreno González De Eiris, Elena
AU  - Álvaro, J.J.
AU  - Vennin, E.
AU  - Perejón, Antonio
AU  - Bechstädt, T.
PY  - 2000
SN  - 1576-5172
UR  - https://hdl.handle.net/20.500.14352/57963
T2  - Geotemas
AB  - In the Esla nappe, three major discontinuities have been recognized within the Lancara Formation. Discontinuity D1 is located at the top of the white bedded limestones. It is recognized as an erosive contact and marks a sharp change from a...
LA  - spa
M2  - 139
PB  - Sociedad Geológica de España
KW  - Sedimentology
KW  - Paleoecology
KW  - Discontinuities
KW  - Cambrian
KW  - Cantabrian Zone
TI  - Discontinuidades sedimentarias en la transición CámbricoInferior-Medio del manto del Esla, Zona Cantábrica
TY  - journal article
VL  - 1
ER  -