Apatite fission track and zircon (U-Th)/HeLow-temperature thermochronology studies have increased our knowledge of the orogenic processes along the Pyrenean-Cantabrian mountain belt by placing time constraints on the exhumation history of its rocks. However, a significant gap of data existed between the Pyrenees and the Cantabrian Mountains, hampering a comprehensive view of the tectonothermal evolution along the belt. Thus, we present a new apatite fission-track (AFT) and zircon (U-Th)/He (ZHe) dataset for the eastern Basque-Cantabrian zone and western Pyrenees. AFT central ages cluster in the Eocene-Oligocene. According to their ZHe age-eU correlations, samples can be separated into two groups: group 1 depicts clustered ZHe ages-eU concen...
International audienceThe Pyrenean belt was formed by the convergence between European and Iberian p...
The Pyrenean-Cantabrian mountain belt extends in an E-W direction along the northern border of Spain...
The Cenozoic evolution of the Pyrenean-Cantabrian mountain belt was driven by both internal andexter...
International audienceAn understanding of the evolution of foreland basins improves our knowledge of...
The Pyrenees represents an orogen that developed diachronously, from east to west, between the Late ...
International audienceWe present new apatite (U–Th)/He (AHe), apatite fission track (AFT) and zircon...
International audienceConstraining the thermal and denudational evolution of continental margins fro...
AbstractWe present new apatite (U–Th)/He (AHe), apatite fission track (AFT) and zircon (U–Th)/He (ZH...
We present new apatite (U-Th)/He (AHe), apatite fission track (AFT) and zircon (U-Th)/He (ZHe) data ...
We present new fission-track and (U–Th)/He data from apatite and zircon in order to reconstruct the ...
The Cenozoic evolution of the Pyrenean-Cantabrian mountain belt was driven by both internal andexter...
The Cenozoic evolution of the Pyrenean-Cantabrian mountain belt was driven by both internal andexter...
International audienceThe Pyrenean belt was formed by the convergence between European and Iberian p...
The Pyrenean-Cantabrian mountain belt extends in an E-W direction along the northern border of Spain...
The Cenozoic evolution of the Pyrenean-Cantabrian mountain belt was driven by both internal andexter...
International audienceAn understanding of the evolution of foreland basins improves our knowledge of...
The Pyrenees represents an orogen that developed diachronously, from east to west, between the Late ...
International audienceWe present new apatite (U–Th)/He (AHe), apatite fission track (AFT) and zircon...
International audienceConstraining the thermal and denudational evolution of continental margins fro...
AbstractWe present new apatite (U–Th)/He (AHe), apatite fission track (AFT) and zircon (U–Th)/He (ZH...
We present new apatite (U-Th)/He (AHe), apatite fission track (AFT) and zircon (U-Th)/He (ZHe) data ...
We present new fission-track and (U–Th)/He data from apatite and zircon in order to reconstruct the ...
The Cenozoic evolution of the Pyrenean-Cantabrian mountain belt was driven by both internal andexter...
The Cenozoic evolution of the Pyrenean-Cantabrian mountain belt was driven by both internal andexter...
International audienceThe Pyrenean belt was formed by the convergence between European and Iberian p...
The Pyrenean-Cantabrian mountain belt extends in an E-W direction along the northern border of Spain...
The Cenozoic evolution of the Pyrenean-Cantabrian mountain belt was driven by both internal andexter...