TY  - JOUR
A1  - Ezpeleta, Miguel
A1  - Parra, Mauricio
A1  - Collo, Gilda
A1  - Wunderlin, Cecilia
A1  - Borrego, Angeles G.
A1  - Sobel, Edward
A1  - Glodny, Johannes
T1  - Thermochronometry unveils ancient thermal regimes in the NW Pampean Ranges, Argentina
BT  - from Mesozoic rifting to Miocene flat-slab subduction
JF  - Basin research
N2  - Reconstructing thermal histories in thrust belts is commonly used to infer the age and rates of thrusting and hence the driving mechanisms of orogenesis. 
In areas where ancient basins have been incorporated into the orogenic wedge, a quantitative reconstruction of the thermal history helps distinguish among potential mechanisms responsible for heating events. 

We present such a reconstruction for the Ischigualasto-Villa Union basin in the western Pampean Ranges of Argentina, where Triassic rifting and late Cretaceous-Cenozoic retroarc foreland basin development has been widely documented, including Miocene flat-slab subduction. 
We report results of organic and inorganic thermal indicators acquired along three stratigraphic sections, including vitrinite reflectance and X-ray diffractometry in claystones and new thermochronological [(apatite fission-track and apatite and zircon [U-Th]/He)] analyses. 
Despite up to 5 km-thick Cenozoic overburden and unlike previously thought, the thermal peak in the basin is not due to Cenozoic burial but occurred in the Triassic, associated with a high heat flow of up to 90 mWm(-2) and <2 km of burial, which heated the base of the Triassic strata to similar to 160 degrees C. Following exhumation, attested by the development of an unconformity between the Triassic and Late-Cretaceous-Cenozoic sequences, Cenozoic re-burial increased the temperature to similar to 110 degrees C at the base of the Triassic section and only similar to 50 degrees C 7 km upsection, suggesting a dramatic decrease in the thermal gradient. 

The onset of Cenozoic cooling occurred at similar to 10(-8) Ma, concomitant with sediment accumulation and thus preceding the latest Miocene onset of thrusting that has been independently documented by stratigraphic-cross-cutting relationships. 
We argue that the onset of cooling is associated with lithospheric refrigeration following establishment of flat-slab subduction, leading to the eastward displacement of the asthenospheric wedge beneath the South American plate. 

Our study places time and temperature constraints on flat-slab cooling that calls for a careful interpretation of exhumation signals in thrustbelts inferred from thermochronology only.
KW  - %Ro
KW  - Cenozoic flat-slab
KW  - Ischigualasto-Villa Union Basin
KW  - thermochronological modelling (AFT, AHe and ZHe)
KW  - Triassic rifting
KW  - XRD in the clay fraction
KW  - heat flow
KW  - burial
Y1  - 2022
U6  - https://doi.org/10.1111/bre.12693
SN  - 0950-091X
SN  - 1365-2117
VL  - 34
IS  - 6
SP  - 1983
EP  - 2012
PB  - Wiley
CY  - Hoboken
ER  -