RT Journal Article
T1 Exhumación alpina del bloque morfotectónico Pedriza - La Cabrera (Sierra del Guadarrama, Sistema Central Español): potencialidad de la termocronometría por trazas de fisión en apatitos
T1 Alpine exhumation of the Pedriza - La cabrera morphotectonic block (Sierra del Guadarrama, Spanish Central System): potentiality of fission - track thermochronology in apatite
A1 Sell, I.
A1 Poupeau, G.
A1 Casquet Martín, César
A1 Galindo, Carmen
A1 González Casado, J. M.
AB The principles of Apatite Fission Track Analysis (AFTA), which allows to decipher the time-temperature paths of apatites since their last cooling below about 110°C are given and one example, from a Pedriza - La Cabrera block, is discussed. It is suggested from AFTA that the cooling history of this sample followed three steps: from 45 Ma to 35 Ma, slow cooling at a rate of 2,5 - 5° C/Ma between 110° C and 60° C, followed by a quasi-plateau at 70-80°C up to about 70 Ma ago, where a new cooling episode started, with a mean 6 -7 ° C/Ma cooling rate up to the present time
PB Sociedad Geológica de España
YR 1995
FD 1995
LK http://hdl.handle.net/10272/13518
UL http://hdl.handle.net/10272/13518
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 16 jul 2026