@article{10272/9523, year = {2001}, url = {http://hdl.handle.net/10272/9523}, abstract = {The Lower Cretaceous series of the northern side of the "Páramo de la Lora" is mainly continental fluvial. A detailed analysis of the section outcropping between Cuillas del Valle and Olleros de Paredes Rubias, has revealed fades which can be attributed to transitional continental-marine enviroments. These are horizontally bedded sandstones with oscillation ripples (lagoon and shoreface), and cross-stratified sandstones with backset laminae (tidal). Other cross-stratified sandstones (fluvial channels), laminated lutites (alluvial coastal plain), bivalve sandstones (tidal ?) and lutites with leaves (marsh), make up contemporaneously-related subenvironments. Storm wave action prevailed during the filling of a narrow erosional depression, and tidal action accompanied the later establishment of valleywide sedimentary conditions}, publisher = {Sociedad Geológica de España}, keywords = {Littoral}, keywords = {Tidal facies}, keywords = {Valley fill}, keywords = {Upper Albian}, keywords = {Olleros}, keywords = {La Lora}, title = {Depósitos de transgresión marina del Albiense superior en la serie terrígena del Páramo de la Lora (vertiente norte, Cantabria y Palencia)}, title = {Upper Albian Transgressive marine deposits in the terrigenous series of the "Páramo de la Lora" (northern side, Cantabria and Palencia, Spain)}, author = {Martínez de Rituerto Ibisate, S. and García Mondéjar, Joaquín}, }