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This setting has exerted major controls on geological processes (magmatism, metamorphism, tectonism, etc.) that in turn affect orogenesis (Cediel et al., 2003 Pilger, 1984 Restrepo-Moreno et al., 2019 Taboada et al., 2000 Vinasco et al., 2006). As a result of this geodynamic setting this Andean segment is affected by complex processes of subduction, collision and accretion of exotic terrains (Cediel et al, 2003, 2019 Page et al., 2005 Restrepo and Toussaint, 1988 Taboada et al., 2000). These mountains have evolved where three lithospheric plates, the Nazca, Caribbean, and South American converge (Fig. The Northern Andes of Colombia are represented by a trident-like distribution of sub-parallel mountain ranges, i.e., the Western, Central and Eastern Cordilleras (WC, CC, and EC, respectively).

Thermobarometry data suggest that the crystallization of the Cretaceous intrusions, now at the surface, took place at depths of 8вЂ“13В km confirming the amount of exhumation revealed by low-temperature thermochronology. From 10В Ma the rates changed to 0.3вЂ“0.33В km/Myr with estimated geothermal gradients of 25вЂ“30В вЊ/km. The thermochronology data imply a total of uplift-driven exhumation (i.e., crustal unroofing) in the study area of up to 10В kms since ~50В MaВ at rates of ~0.1В km/Myr and 4В kms since ~23В Ma initially at 0.2В km/Myr. A fourth event, at ~10В Ma, is tentatively recognized in modelled data sets, but not by absolute age values. The latter two phases correlate well with the Pre-Andean and Proto-Andean periods previously identified on the basis of stratigraphic unconformities and thermochronology studies in the region. The results are combined with published apatite (UвЂ“Th)/He ages revealing three episodes of increased cooling during the Late Cretaceous (~110 - 90В Ma), the Eocene (~55-40В Ma) and the Miocene (23-20В Ma).

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*Some exceptions may apply, please click return and refundsfor full details on items that are non-returnable.New zircon and apatite fission-track analyses and aluminium in hornblende thermobarometric data are presented from Cretaceous and Triassic plutons situated along an east-west transect across the Central Cordillera, the Cauca Romeral Fault System and the eastern slopes of the Western Cordillera in the Colombian Andes. For details on returns for all other regions click here Returns Policy EU returns are charged at a flat rate of ВЈ4.

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