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- W2890364695 abstract "The history of exhumation and denudation of the Cenozoic St. Elias orogen is stored in the sediments of the Miocene to Holocene Surveyor Fan, Gulf of Alaska. The orogeny of the mountain belt coincides with major climatic events leading to varying degrees of glaciation that are considered to have strongly interacted with mountain-building processes. In order to assess the relative influence of climate and tectonics on erosion patterns and to reconstruct sediment routing to the ocean, we combine zircon U-Pb dating and (U-Th)/He thermochronology with analysis of rare earth elements and Hf isotopes of zircons of sands and silts from Integrated Ocean Drilling Program expedition 341 sites U1417 and U1418 in the Surveyor Fan. All Miocene to Pleistocene sediments show similar U-Pb age spectra, indicating that the main source areas remained the same during different stages of glaciation. A prominent age component at 50–60 Ma can be linked to the Chugach Metamorphic Complex and the Sanak-Baranof plutonic belt in the mountain range. Older grains can be referred to low-grade metamorphic sources within the Chugach, Prince William, and Yakutat terranes. A decrease in 50–60 Ma igneous and metamorphic zircons implies a reduction of input from the Chugach Metamorphic Complex and the Sanak-Baranof plutonic belt. This indicates that the southward advance of glaciers toward the ocean, together with tectonic changes from the Miocene to the Pliocene, triggered a higher contribution from the newly glaciated areas. During times of increased glaciation in the Pleistocene, glaciers appear to have been nested in the same area as before. Our data do not give evidence of a general change in the drainage systems or the tectonic setting during the Pleistocene but also do not prove the absence of such." @default.
- W2890364695 created "2018-09-27" @default.
- W2890364695 creator A5001296471 @default.
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- W2890364695 date "2018-11-01" @default.
- W2890364695 modified "2023-09-27" @default.
- W2890364695 title "Provenance of the Surveyor Fan and Precursor Sediments in the Gulf of Alaska—Implications of a Combined U-Pb, (U-Th)/He, Hf, and Rare Earth Element Study of Detrital Zircons" @default.
- W2890364695 cites W1638349272 @default.
- W2890364695 cites W1847352453 @default.
- W2890364695 cites W1863224392 @default.
- W2890364695 cites W1871734886 @default.
- W2890364695 cites W1964522987 @default.
- W2890364695 cites W1965832621 @default.
- W2890364695 cites W1987733382 @default.
- W2890364695 cites W1988828197 @default.
- W2890364695 cites W1991905364 @default.
- W2890364695 cites W1994004159 @default.
- W2890364695 cites W1996934717 @default.
- W2890364695 cites W1999621813 @default.
- W2890364695 cites W2000953417 @default.
- W2890364695 cites W2002460023 @default.
- W2890364695 cites W2007105153 @default.
- W2890364695 cites W2007525743 @default.
- W2890364695 cites W2008451537 @default.
- W2890364695 cites W2009732140 @default.
- W2890364695 cites W2011050884 @default.
- W2890364695 cites W2017847201 @default.
- W2890364695 cites W2020298416 @default.
- W2890364695 cites W2020973699 @default.
- W2890364695 cites W2021794238 @default.
- W2890364695 cites W2022310117 @default.
- W2890364695 cites W2023941853 @default.
- W2890364695 cites W2029013584 @default.
- W2890364695 cites W2029277152 @default.
- W2890364695 cites W2029743607 @default.
- W2890364695 cites W2030464689 @default.
- W2890364695 cites W2030958259 @default.
- W2890364695 cites W2031960462 @default.
- W2890364695 cites W2039872199 @default.
- W2890364695 cites W2041226839 @default.
- W2890364695 cites W2043549449 @default.
- W2890364695 cites W2048857036 @default.
- W2890364695 cites W2049657152 @default.
- W2890364695 cites W2053514714 @default.
- W2890364695 cites W2054454047 @default.
- W2890364695 cites W2059356468 @default.
- W2890364695 cites W2062862625 @default.
- W2890364695 cites W2068397892 @default.
- W2890364695 cites W2073326270 @default.
- W2890364695 cites W2080325016 @default.
- W2890364695 cites W2080982161 @default.
- W2890364695 cites W2084701616 @default.
- W2890364695 cites W2085383211 @default.
- W2890364695 cites W2085487451 @default.
- W2890364695 cites W2088194408 @default.
- W2890364695 cites W2089832042 @default.
- W2890364695 cites W2091019729 @default.
- W2890364695 cites W2093067863 @default.
- W2890364695 cites W2093326692 @default.
- W2890364695 cites W2093369526 @default.
- W2890364695 cites W2101245568 @default.
- W2890364695 cites W2103178332 @default.
- W2890364695 cites W2107360734 @default.
- W2890364695 cites W2111180855 @default.
- W2890364695 cites W2120451076 @default.
- W2890364695 cites W2126352160 @default.
- W2890364695 cites W2128610717 @default.
- W2890364695 cites W2131587907 @default.
- W2890364695 cites W2132177541 @default.
- W2890364695 cites W2136813788 @default.
- W2890364695 cites W2137556997 @default.
- W2890364695 cites W2137919069 @default.
- W2890364695 cites W2138250703 @default.
- W2890364695 cites W2139643162 @default.
- W2890364695 cites W2145180142 @default.
- W2890364695 cites W2156907569 @default.
- W2890364695 cites W2156985625 @default.
- W2890364695 cites W2161838140 @default.
- W2890364695 cites W2164698976 @default.
- W2890364695 cites W2168176243 @default.
- W2890364695 cites W2171662275 @default.
- W2890364695 cites W2175570416 @default.
- W2890364695 cites W2251914726 @default.
- W2890364695 cites W2270737667 @default.
- W2890364695 cites W2309961263 @default.
- W2890364695 cites W2318409896 @default.
- W2890364695 cites W2342124398 @default.
- W2890364695 cites W2398605979 @default.
- W2890364695 cites W2515228057 @default.
- W2890364695 cites W2530683126 @default.
- W2890364695 cites W2546450222 @default.
- W2890364695 cites W2571294349 @default.
- W2890364695 cites W2580269748 @default.
- W2890364695 cites W2592262461 @default.
- W2890364695 cites W2614937491 @default.