T164 Recent Advances in Understanding Magmatism along and within the Northern North American Cordillera (Posters)
Monday, 26 September 2016
9:00 AM - 6:30 PM
Exhibit Hall E/F
GEOLOGICAL EVIDENCE FROM THE DOONERAK FENSTER AND THE ENDICOTT MOUNTAINS ALLOCHTHON OF THE CENTRAL BROOKS RANGE, ALASKA: INSIGHTS INTO THE ASSEMBLY OF THE ARCTIC ALASKA TERRANE
Paper number: T164-9
Program: Technical Sessions
Time: 9:00 AM – 6:30 PM
Authors
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Benjamin JohnsonWest Virginia University, Morgantown, WV
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Jaime ToroWest Virginia University, Morgantown, WV
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Greg HammondWest Virginia University, Morgantown, WV
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Justin StraussDartmouth College, Hanover, NH
Abstract
New whole-rock major and trace element geochemical analyses conducted on the Apoon volcanic rocks show somewhat variable patterns, but all samples are consistent with an arc/subduction-related tectonic setting. U-Pb detrital zircon ages from volcaniclastic portions of the Apoon assemblage highlight a prominent unimodal 440-530 Ma population, which is in concert with previous U-Pb geochronology from the Apoon assemblage. A similar prominent detrital population is present in the siliciclastic units of the Endicott Mountains allochthon. This could imply that the Endicott Mountains allochthon units were sourced by recycling the volcanic and volcaniclastic rocks of the Apoon assemblage; however, the allochthonous units bear detrital populations that are absent within the Apoon assemblage and are similar to those seen along the Canadian Arctic Islands, Svalbard, eastern Greenland, and possibly northern Baltica. This recorded shift in provenance likely corresponds with the closure of the northern Iapetus Ocean and the amalgamation of the Arctic Alaska terrane.
Geological Society of America Abstracts with Programs. Vol. 48, No. 7
doi: 10.1130/abs/2016AM-287987
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