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- W2588551485 abstract "We present an integrated study of the postcollisional (post–Late Jurassic) history of the Blue Mountains province (Oregon and Idaho, USA) using constraints from Cretaceous igneous and sedimentary rocks. The Blue Mountains province consists of the Wallowa and Olds Ferry arcs, separated by forearc accretionary material of the Baker terrane. Four plutons (Lookout Mountain, Pedro Mountain, Amelia, Tureman Ranch) intrude along or near the Connor Creek fault, which separates the Izee and Baker terranes. High-precision U-Pb zircon ages indicate 129.4–123.8 Ma crystallization ages and exhibit a north-northeast–younging trend of the magmatism. The 40Ar/39Ar analyses on biotite and hornblende indicate very rapid (<1 m.y.) cooling below biotite closure temperature (∼350 °C) for the plutons. The (U-Th)/He zircon analyses were done on a series of regional plutons, including the Lookout Mountain and Tureman Ranch plutons, and indicate a middle Cretaceous age of cooling through ∼200 °C. Sr, Nd, and Pb isotope geochemistry on the four studied plutons confirms that the Izee terrane is on Olds Ferry terrane basement. We also present data from detrital zircons from Late Cretaceous sedimentary rocks at Dixie Butte, Oregon. These detrital zircons record only Paleozoic–Mesozoic ages with only juvenile Hf isotopic compositions, indicating derivation from juvenile accreted terrane lithosphere. Although the Blue Mountains province is juxtaposed against cratonic North America along the western Idaho shear zone, it shows trends in magmatism, cooling, and sediment deposition that differ from the adjacent part of North America and are consistent with a more southern position for terranes of this province at the time of their accretion. We therefore propose a tectonic history involving moderate northward translation of the Blue Mountains province along the western Idaho shear zone in the middle Cretaceous." @default.
- W2588551485 created "2017-02-24" @default.
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- W2588551485 date "2017-02-14" @default.
- W2588551485 modified "2023-10-16" @default.
- W2588551485 title "Intrusive and depositional constraints on the Cretaceous tectonic history of the southern Blue Mountains, eastern Oregon" @default.
- W2588551485 cites W1507427626 @default.
- W2588551485 cites W1517251788 @default.
- W2588551485 cites W1669138304 @default.
- W2588551485 cites W1676801909 @default.
- W2588551485 cites W1898112109 @default.
- W2588551485 cites W1952639126 @default.
- W2588551485 cites W1969859799 @default.
- W2588551485 cites W1972019729 @default.
- W2588551485 cites W1973671106 @default.
- W2588551485 cites W1981015190 @default.
- W2588551485 cites W1981100101 @default.
- W2588551485 cites W1984121331 @default.
- W2588551485 cites W1990455253 @default.
- W2588551485 cites W1998101266 @default.
- W2588551485 cites W2002178446 @default.
- W2588551485 cites W2005014931 @default.
- W2588551485 cites W2006382076 @default.
- W2588551485 cites W2008009942 @default.
- W2588551485 cites W2013883793 @default.
- W2588551485 cites W2015419319 @default.
- W2588551485 cites W2017775719 @default.
- W2588551485 cites W2018449004 @default.
- W2588551485 cites W2020304604 @default.
- W2588551485 cites W2024809013 @default.
- W2588551485 cites W2028647203 @default.
- W2588551485 cites W2030958259 @default.
- W2588551485 cites W2031398064 @default.
- W2588551485 cites W2032803594 @default.
- W2588551485 cites W2038301567 @default.
- W2588551485 cites W2040150234 @default.
- W2588551485 cites W2043700280 @default.
- W2588551485 cites W2049942662 @default.
- W2588551485 cites W2052305024 @default.
- W2588551485 cites W2061278087 @default.
- W2588551485 cites W2062491474 @default.
- W2588551485 cites W2064536421 @default.
- W2588551485 cites W2067964439 @default.
- W2588551485 cites W2068717220 @default.
- W2588551485 cites W2071362208 @default.
- W2588551485 cites W2071613015 @default.
- W2588551485 cites W2072405676 @default.
- W2588551485 cites W2075033609 @default.
- W2588551485 cites W2075694434 @default.
- W2588551485 cites W2078687304 @default.
- W2588551485 cites W2081343432 @default.
- W2588551485 cites W2084955401 @default.
- W2588551485 cites W2091479516 @default.
- W2588551485 cites W2092304740 @default.
- W2588551485 cites W2094182452 @default.
- W2588551485 cites W2103004682 @default.
- W2588551485 cites W2105662998 @default.
- W2588551485 cites W2106311459 @default.
- W2588551485 cites W2108281812 @default.
- W2588551485 cites W2110464369 @default.
- W2588551485 cites W2114203981 @default.
- W2588551485 cites W2124479594 @default.
- W2588551485 cites W2128808897 @default.
- W2588551485 cites W2132689042 @default.
- W2588551485 cites W2138952581 @default.
- W2588551485 cites W2139191262 @default.
- W2588551485 cites W2139788788 @default.
- W2588551485 cites W2142587932 @default.
- W2588551485 cites W2144080774 @default.
- W2588551485 cites W2145087726 @default.
- W2588551485 cites W2145758959 @default.
- W2588551485 cites W2145898590 @default.
- W2588551485 cites W2146613895 @default.
- W2588551485 cites W2149600508 @default.
- W2588551485 cites W2151978486 @default.
- W2588551485 cites W2155895997 @default.
- W2588551485 cites W2159307678 @default.
- W2588551485 cites W2161909354 @default.
- W2588551485 cites W2164468447 @default.
- W2588551485 cites W2167572891 @default.
- W2588551485 cites W2168176243 @default.
- W2588551485 cites W2263541286 @default.
- W2588551485 cites W2284950925 @default.
- W2588551485 cites W2306789206 @default.
- W2588551485 cites W2312320844 @default.
- W2588551485 cites W2330720274 @default.
- W2588551485 cites W2334367703 @default.
- W2588551485 cites W2480055599 @default.
- W2588551485 cites W2509291758 @default.