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The Meshik Arc: An eocene to earliest miocene magmatic arc on the Alaska Peninsula

December 31, 1985

The Meshik arc is herein defined to include Eocene to earliest Miocene volcanic and hypabyssal rocks and the associated Meshik and Stepovak Formations of the central Alaska Peninsula. Igneous rocks range from basalt to dacite and yielded K-Ar ages of 48 to 22 m.y. The Meshik arc is oriented along the trend of the Alaska Peninsula, subparallel to the present-day Aleutian arc. Rocks of the Meshik arc are emplaced on Cenozoic, Mesozoic, and older clastic sedimentary rocks of the Alaska Peninsula terrane. Tectonic interpretation suggests: a) the arc represents a relatively stationary period in the otherwise mobile migration of the Alaska Peninsula terrane, b) subduction was an important process along the Alaska Peninsula during Tertiary time, and c) most migration of the Alaska Peninsula terrane since Cretaceous time took place in Paleocene and middle Miocene time.

Publication Year 1985
Title The Meshik Arc: An eocene to earliest miocene magmatic arc on the Alaska Peninsula
DOI 10.14509/2269
Authors Frederic H. Wilson
Publication Type Report
Publication Subtype State or Local Government Series
Series Title Alaska Division of Geological & Geophysical Surveys Professional Reports
Series Number DGGS PR 88
Index ID 70187739
Record Source USGS Publications Warehouse
USGS Organization Alaska Science Center