Evolution of a Permo-Triassic sedimentary melange, Grindstone terrane, east-central Oregon

Geological Society of America Bulletin
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Abstract

The Grindstone terrane in east-central Oregon is one of the few areas in western North America where large blocks of unmetamorphosed Devonian, Mississippian, and Permian limestones are inter mixed with Permian and Lower Triassic radiolarian chert and Pennsylvanian?, Permian, and Triassic volcaniclastic rocks. Although originally described as parts of a coherent succession, we interpret the Grindstone rocks to be a sedimentary mélange composed of Paleozoic limestone slide and slump blocks that became detached from a carbonate shelf fringing a volcanic knoll or edifice in Late Permian to Middle Triassic time and were intermixed with Permian and Triassic slope to basinal clastic and volcaniclastic rocks in a forearc basin setting. Paleogeographic affinities of the Grindstone limestone faunas and volcaniclastic debris in the limestone and clastic rocks all indicate deposition in proximity to an island-arc system near the North American craton. The Grindstone terrane deposits are unconformably overlain by Upper Triassic to Middle Jurassic sequences of the Izee terrane. Although lithologic and faunal differences indicate that the Grindstone and Izee terranes together represent a tectonic block separate from the adjacent Baker terrane, all three terranes were juxtaposed by Late Triassic or Early Jurassic time.

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Publication type Article
Publication Subtype Journal Article
Title Evolution of a Permo-Triassic sedimentary melange, Grindstone terrane, east-central Oregon
Series title Geological Society of America Bulletin
DOI 10.1130/0016-7606(1991)103<1280:EOAPTS>2.3.CO;2
Volume 103
Issue 10
Year Published 1991
Language English
Publisher Geological Society of America
Description 17 p.
First page 1280
Last page 1296
Country United States
State Oregon
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