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- W2908069372 endingPage "469" @default.
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- W2908069372 abstract "Constraining the way in which continental deformation is accommodated in time and space is essential to reconcile past plate movements with geological observations. Kinematic reconstructions of the Iberia-Europe plate boundary are still debated. Here we focus on an inverted Mesozoic rift basin, the Cameros basin, which is part of the Iberian chain. We use a combination of detrital low-temperature thermochronological techniques to define the time-temperature evolution of the basin from Mesozoic rifting to Cenozoic collision. Zircon fission-track analyses of Oligocene–Miocene sedimentary rocks yield two main age populations at ~170 ± 10 and ~100 ± 10 Ma, reflecting (i) an Early Jurassic thermal event related to the Atlantic-Alpine Tethys opening and (ii) an Albo-Cenomanian thermal event related to the Bay of Biscay opening. Thermal modeling of combined zircon fission-track, apatite fission-track, and apatite (U-Th-Sm)/He data reveals that collision-related cooling of the Cameros basin started during the Paleocene (~60 Ma). A second cooling/exhumation phase of the basin is recorded from 35 to 25 Ma. Initial cooling occurred after a protracted postrift period characterized by persistence of high geothermal gradients, a feature also recognized in the Pyrenees. Our results show that the Iberian chain shared the same Early to Late Jurassic tectonothermal evolution with the Atlantic-Alpine Tethyan rifted margins. From the Albian onward, the thermal evolution of the Cameros basin was very similar to that of the Pyrenees. This study shows that the preservation in mountain ranges of a succession of rifting events provide important clues for plate reconstructions." @default.
- W2908069372 created "2019-01-11" @default.
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- W2908069372 creator A5080792534 @default.
- W2908069372 date "2019-02-01" @default.
- W2908069372 modified "2023-10-09" @default.
- W2908069372 title "Tectonothermal Evolution of the Cameros Basin: Implications for Tectonics of North Iberia" @default.
- W2908069372 cites W1498314499 @default.
- W2908069372 cites W1529788327 @default.
- W2908069372 cites W1538361609 @default.
- W2908069372 cites W1551215360 @default.
- W2908069372 cites W155180398 @default.
- W2908069372 cites W1635581289 @default.
- W2908069372 cites W1650719564 @default.
- W2908069372 cites W1687675348 @default.
- W2908069372 cites W1835607377 @default.
- W2908069372 cites W1860912165 @default.
- W2908069372 cites W187002222 @default.
- W2908069372 cites W1889975196 @default.
- W2908069372 cites W1932542429 @default.
- W2908069372 cites W1960465926 @default.
- W2908069372 cites W1964631208 @default.
- W2908069372 cites W1970296230 @default.
- W2908069372 cites W1970365532 @default.
- W2908069372 cites W1974140605 @default.
- W2908069372 cites W1974297197 @default.
- W2908069372 cites W1975326207 @default.
- W2908069372 cites W1980216110 @default.
- W2908069372 cites W1987085354 @default.
- W2908069372 cites W1988019811 @default.
- W2908069372 cites W1988411879 @default.
- W2908069372 cites W1988657625 @default.
- W2908069372 cites W1988719706 @default.
- W2908069372 cites W1994241992 @default.
- W2908069372 cites W1994609458 @default.
- W2908069372 cites W1995483270 @default.
- W2908069372 cites W1995973065 @default.
- W2908069372 cites W1996405470 @default.
- W2908069372 cites W1996785858 @default.
- W2908069372 cites W2001788443 @default.
- W2908069372 cites W2004810036 @default.
- W2908069372 cites W2006040444 @default.
- W2908069372 cites W2006505221 @default.
- W2908069372 cites W2007759357 @default.
- W2908069372 cites W2007858403 @default.
- W2908069372 cites W2013390827 @default.
- W2908069372 cites W2014375628 @default.
- W2908069372 cites W2020001694 @default.
- W2908069372 cites W2020022047 @default.
- W2908069372 cites W2021444397 @default.
- W2908069372 cites W2028032600 @default.
- W2908069372 cites W2038907414 @default.
- W2908069372 cites W2042366312 @default.
- W2908069372 cites W2046605699 @default.
- W2908069372 cites W2048674039 @default.
- W2908069372 cites W2050258118 @default.
- W2908069372 cites W2051819341 @default.
- W2908069372 cites W2059328863 @default.
- W2908069372 cites W2059401764 @default.
- W2908069372 cites W2059747435 @default.
- W2908069372 cites W2064065757 @default.
- W2908069372 cites W2065898420 @default.
- W2908069372 cites W2065933321 @default.
- W2908069372 cites W2066886350 @default.
- W2908069372 cites W2068244503 @default.
- W2908069372 cites W2068892745 @default.
- W2908069372 cites W2070847564 @default.
- W2908069372 cites W2071579631 @default.
- W2908069372 cites W2071743163 @default.
- W2908069372 cites W2073350342 @default.
- W2908069372 cites W2080847251 @default.
- W2908069372 cites W2081617724 @default.
- W2908069372 cites W2083244895 @default.
- W2908069372 cites W2083260737 @default.
- W2908069372 cites W2087900760 @default.
- W2908069372 cites W2092464849 @default.
- W2908069372 cites W2092805274 @default.
- W2908069372 cites W2094180430 @default.
- W2908069372 cites W2105792028 @default.
- W2908069372 cites W2107249261 @default.
- W2908069372 cites W2108610660 @default.
- W2908069372 cites W2112130030 @default.
- W2908069372 cites W2115733899 @default.
- W2908069372 cites W2116351028 @default.
- W2908069372 cites W2123430617 @default.
- W2908069372 cites W2123464034 @default.
- W2908069372 cites W2125403926 @default.
- W2908069372 cites W2135709313 @default.
- W2908069372 cites W2136913787 @default.
- W2908069372 cites W2139326036 @default.
- W2908069372 cites W2146093540 @default.