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A detrital record of Mesozoic island arc accretion and exhumation in the North American Cordillera: U‐Pb geochronology of the Kahiltna basin, southern Alaska
Author(s) -
Hampton Brian A.,
Ridgway Kenneth D.,
Gehrels George E.
Publication year - 2010
Publication title -
tectonics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.465
H-Index - 134
eISSN - 1944-9194
pISSN - 0278-7407
DOI - 10.1029/2009tc002544
Subject(s) - geology , cretaceous , terrane , detritus , zircon , precambrian , paleontology , mesozoic , geochronology , accretion (finance) , provenance , paleozoic , structural basin , tectonics , physics , astrophysics
The stratigraphic record of Mesozoic arc accretion in the North American Cordillera is preserved in a discontinuous belt of clastic strata that are exposed inboard (cratonward) of the allochthonous Wrangellia composite terrane in southern Alaska, western Canada, and Washington State. LA‐ICPMS analyses of eight samples (n = 714 detrital zircon grains) collected at different stratigraphic intervals from the Jurassic‐Cretaceous Kahiltna assemblage in southern Alaska reveals a bulk U‐Pb age distribution of Precambrian‐Mesozoic age grains (Mz 74%, Pz 11%, Pc 15%). A comparison of U‐Pb ages from older to younger stratigraphic intervals within the Kahiltna assemblage reveals three stages of exhumation and basin development during arc accretion. Stages include (1) an initial Late Jurassic–Early Cretaceous pre/early collisional phase during which detritus was derived almost solely from Middle–Late Jurassic and Early Cretaceous magmatic sources of the outboard Wrangellia composite terrane (Mz 100%, Pz 0%, Pc, 0%), (2) a second Early Cretaceous syncollisional phase that reflects the introduction of Paleozoic and Precambrian detritus from the inboard Intermontane belt (Mz 84%, Pz 11%, Pc 5%) and an upsection increase in older detrital zircon grains compared to Mesozoic age grains (Mz 65%, Pz 11%, Pc 24%), and (3) a final Early‐Late Cretaceous late/postcollisional phase that represents continued detrital contributions from Precambrian–Mesozoic source areas (Mz 19%, Pz 22%, Pc 59%) located inboard and outboard of the Kahiltna basin. Similar bulk trends in detrital zircon age populations have been reported from along‐strike, age‐equivalent strata of the Gravina belt (Mz 74%, Pz 20%, Pc 6%) in southeastern Alaska suggesting that similar provenance trends may exist in basins along this >2000 km ‐long collisional zone.