Apatite fission-track and (U-Th)/He ages from Carboniferous to Eocene siliciclastic rocks of the Istanbul Zone (NW Turkey) range from 220 to 46 Ma, and from 46 to 18 Ma, respectively. Apatite grains f
Supporting information for the Geochemistry, Geophysics, Geosystems - AGU Publications manuscript: "High-resolution P-T-time paths across Himalayan faults exposed along the Bhagirathi Transect NW Indi
The amalgamation of Pangea during the Carboniferous produced a winding mountain belt: the Variscan orogen of West Europe. In the Iberian Peninsula, this tortuous geometry is dominated by two major str
