RT Journal Article
T1 Cortejos sedimentarios en parasecuencias de 4e y 5S orden en el Cenomaniense de la rama aragonesa de la Cordillera Ibérica (España)
T1 Systems Tracts in 4th and 5th order parasequences in the Cenomanian of the Aragonian branch of the Iberian Ranges (Spain)
A1 García Hidalgo, J. F.
A1 Segura, M.
A1 García, A.
A1 Ruiz, G.
AB Parasequences Jn the Upper Albian-Cenomanian of the Iberian Ranges are deepening and then shallowing upwards parasequences, in opposition to standard parasequences which shallow upwards. They were originated by cycles of relative rise and fall of the sea level and then Systems Tracts (LST, TST and HST) can be recognisedas in 3rd order sequences. Superimposition of Systems Tracts occur and usually a 3rd order HST is composed by parasequences including all lowstand, transgressive and highsland Systems Tracts. In basin analysis that superimposition originates that lowstand facies, such as slope breccias, can be originated during 3rd order highstands in relation to high frequency (4th and 5th order) relative sea level falls
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/11373
UL http://hdl.handle.net/10272/11373
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 13 jun 2026