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Title: Jurassic tectonic wedging and crustal block rotation, northern Sierra Nevada California

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5022281
;  [1]
  1. Geological Survey, Menlo Park, CA (United States)

Rocks in the northern Sierra Nevada east of the Feather River peridotite belt (FRPB) and south of 39[degree]45 minutes N. strike NNW, dip steeply E and form an east-facing homoclinal section as much as 35km thick. The lower Paleozoic Shoo Fly Complex (SFC), the oldest and western-most unit in the homoclinal section, is faulted against the FRPB. Middle Jurassic volcanic rocks (Jv) at the top of the homoclinal section are down-faulted against Paleozoic rocks to the east along the Talbot fault (TF). A positive aeromagnetic anomaly and east-sloping gradient south of 39[degree]45 minutes N. indicate that the east contact of the FRPB dips about 45[degree]E. beneath the homoclinal section and extends to a depth of at least 10km. The contact between the buried FRPB and the homoclinal section is interpreted to be the roof thrust of an east-tapering wedge of serpentinized oceanic crust and upper mantle, probably emplaced in the Early and Middle Jurassic. Normal, west-down displacement on the Talbot fault, contemporaneous with east-vergent edging, resulted in eastward block rotation of the rocks above the wedge, syndepositional thickening of the Early and Middle Jurassic Sailor Canyon Formation (Jsc) relative to the coeval rocks east of the Talbot fault, and structural control for Middle Jurassic magmatism.

OSTI ID:
5022281
Report Number(s):
CONF-9305259-; CODEN: GAAPBC
Journal Information:
Geological Society of America, Abstracts with Programs; (United States), Vol. 25:5; Conference: 89. annual meeting of the Cordilleran Section and the 46th annual meeting of the Rocky Mountain Section of the Geological Society of America (GSA), Reno, NV (United States), 19-21 May 1993; ISSN 0016-7592
Country of Publication:
United States
Language:
English