In the Racó Llobet section (Sierra Mariola, Prebetic of Alicante) crops out the Llopis Formation, dated as lower Aptian (lower Bedoulian). Six types of facies have been recognized: 1) orbitolinite facies (packstone and wackestone with orbitolinids); 2) calcarenites with grainstone texture; 3) limestones and marlstones with corals; 4) floatstones and packstones with rudists; 5) wackestone and packstone with foraminifera; and 6) mudstone with scarce fossils. These facies correspond with shallowing upward elementary cycles. In general, this section records the process of installation of a shallow carbonate platform, occurred in two progradational steps, ending with the development of a lagoonEn la sección de Racó Llobet (Sierra Mariol...
At 32° 40′ south latitude the Andean orogen shows a typical thin-skinned fold and thrust belt that e...
The autors paint out the sedimentary characteristics of the lower member of the Pedroche Formation (...
There is in this note a facies description of the upper Cre- taceous clay levels with corals from Po...
The Aptian stratigraphic record of the Alicante region consists of: a rudist and coral-rich carbonat...
The materials from Miocene age which appeared in this area are attributed to the so-ca/led «post-man...
This paper focuses in the sedimentary history during the upper Aptian of the distensive Organyà Basi...
El Palegeóno aflorante en la Sierra de Tramuntana muestra la existencia de dos unidades litoestratig...
The study of several sections on platform limestones of Aptian-Albian age in SE Spain (Alicante prov...
En la Sierra de la Estrella (Área del Guadiato, Córdoba) se localiza una sucesión del Viseense super...
The Pliensbachian of the Aragonese branch of the Iberian Chain is represented by Almonacid de la Cub...
The Sierra del Castell de la Solana (NE Alicante province) exhibits a thick section (about 750 m ) o...
El presente trabajo muestra la caracterización en detalle de la secuencia estratigráfica de los depó...
Se han estudiado las variaciones de facies sedimentarias en una sucesión albiense de calizas somera...
11 páginas, 5 figuras.[ES] En el Keuper inferior del sector central de la Cordillera Bética hay un...
Sedimentological and petrological analysis of the Gorafe-Huélago formation (pliocene) permits to dis...
At 32° 40′ south latitude the Andean orogen shows a typical thin-skinned fold and thrust belt that e...
The autors paint out the sedimentary characteristics of the lower member of the Pedroche Formation (...
There is in this note a facies description of the upper Cre- taceous clay levels with corals from Po...
The Aptian stratigraphic record of the Alicante region consists of: a rudist and coral-rich carbonat...
The materials from Miocene age which appeared in this area are attributed to the so-ca/led «post-man...
This paper focuses in the sedimentary history during the upper Aptian of the distensive Organyà Basi...
El Palegeóno aflorante en la Sierra de Tramuntana muestra la existencia de dos unidades litoestratig...
The study of several sections on platform limestones of Aptian-Albian age in SE Spain (Alicante prov...
En la Sierra de la Estrella (Área del Guadiato, Córdoba) se localiza una sucesión del Viseense super...
The Pliensbachian of the Aragonese branch of the Iberian Chain is represented by Almonacid de la Cub...
The Sierra del Castell de la Solana (NE Alicante province) exhibits a thick section (about 750 m ) o...
El presente trabajo muestra la caracterización en detalle de la secuencia estratigráfica de los depó...
Se han estudiado las variaciones de facies sedimentarias en una sucesión albiense de calizas somera...
11 páginas, 5 figuras.[ES] En el Keuper inferior del sector central de la Cordillera Bética hay un...
Sedimentological and petrological analysis of the Gorafe-Huélago formation (pliocene) permits to dis...
At 32° 40′ south latitude the Andean orogen shows a typical thin-skinned fold and thrust belt that e...
The autors paint out the sedimentary characteristics of the lower member of the Pedroche Formation (...
There is in this note a facies description of the upper Cre- taceous clay levels with corals from Po...