RT Journal Article
T1 Tempestitas en el Subbético medio (Fm. Milanos, Jurásico superior). Sus características y facies relacionadas
T1 Tempestites in the Middle Subbetic (Milanos Fm, Upper Jurassic). Their characterístics and related facies
A1 Molina, José Miguel
A1 Vera, J. A.
AB We have recognized and analysed tempestites, made up by calcisiltites and calcarenites with chert and hummocky cross-stratification (HCS), in the Milanos Fm (Upper Jurassic) of the Middle Subbetic (Betic Cordillera). The most characteristic calcareous tempestite levels are packstone and grainstone (more rarely wackestone) with peloids and bioclasts. They have a thickness between 25 to 75 cm and a distinctive elemental sequence. The presence of these tempestite levels is a fundamental new argument to interpret these deposits as characteristics of the deeper parts of a platform or carbonate outer ramp, less than 200 m in depth
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/12215
UL http://hdl.handle.net/10272/12215
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 15 jun 2026