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Preliminary description of the Late Silurian-Early Devonian Klakas Orogeny in the southern Alexander terrane, southeastern Alaska

Gehrels, George E. and Saleeby, Jason B. and Berg, Henry C. (1983) Preliminary description of the Late Silurian-Early Devonian Klakas Orogeny in the southern Alexander terrane, southeastern Alaska. In: Pre-Jurassic rocks in western North American suspect terranes. Society of Economic Paleontologists and Mineralogists , Los Angeles, CA, pp. 131-141.

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The Klakas orogeny is a Late Silurian-Early Devonian deformational, metamorphic, and mountain-building event that marks a major change in the geologic history of the southern Alexander terrane. During Ordovician-Silurian time this region was a marine volcano-plutonic province in which volcani-clastic strata and shallow-water limestones were deposited adjacent to andesitic and dacitic volcanic centers. After the Klakas orogeny, shallow-marine sedimentation prevailed with only local volcanism. Manifestations of this orogenic event included: 1) shallow-level brecciation of Ordovician-Silurian rocks on southern Prince of Wales Island, 2) deformation along with greenschist- and perhaps amphibolite-facies metamorphism of Ordovician-Silurian rocks on Annette and Gravina Islands, 3) structural uplift of at least several kilometers during or shortly after the deformation, 4) uplift of mountainous areas with kilometer-scale topographic relief, and 5) deposition of a subaerial to shallow-marine elastic wedge that was shed from these uplifted areas. Reconstructions of the paleogeography and tectonic history of the Alexander terrane during Ordovician through Devonian time reveal that: 1) the eastern (Annette) and western (Craig) subterranes of the Alexander terrane are part of the same tectonic fragment, 2) the deformational fabrics in Paleozoic rocks in the southern part of the terrane are primarily Late Silurian-Early Devonian in age, and not a product of the Late Cretaceous accretion of the terrane, and 3) northeastern Chichagof Island may have been adjacent to southern Prince of Wales Island during Silurian-Devonian time, which suggests that the Chatham Strait fault and related fault systems may have approximately 350 km of post-Devonian right-slip displacement.

Item Type:Book Section
Additional Information:© 1983 Society of Economic Paleontologists and Mineralogists. Our studies in southeastern Alaska have been funded by the U.S. Geological Survey, with additional financial assistance awarded to Gehrels from the California Institute of Technology, the Geological Society of America, and Sigma Xi. We would like to thank these organizations for their support. The assistance of Ryan Turner, Bill McClelland and Karl Mueller in the field is also much appreciated. David A. Brew provided a thorough and very helpful review of an early version of this manuscript. This is California Institute of Technology contribution number 3888.
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Geological Society of AmericaUNSPECIFIED
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Caltech Division of Geological and Planetary Sciences3888
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ID Code:53895
Deposited By: Tony Diaz
Deposited On:20 Jan 2015 22:17
Last Modified:03 Oct 2019 07:53

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