Sj. Wyld, EARLY JURASSIC DEFORMATION IN THE PINE FOREST RANGE, NORTHWEST NEVADA, AND IMPLICATIONS FOR CORDILLERAN TECTONICS, Tectonics, 15(3), 1996, pp. 566-583
Triassic and Jurassic rocks in the Black Rock Desert of northwest Neva
da comprise part of the Mesozoic volcanic are successions found throug
hout the westernmost U.S. Cordillera. Detailed structural studies in t
he fine Forest Range, located in the western Black Rock: Desert, provi
de new insight into the Jurassic structural history of this part of th
e Mesozoic are system. Regional Jurassic deformation and metamorphism
in the Fine Forest Range affected a thick (similar to 10.5 km) section
of lower(?) Paleozoic through Triassic strata that were tilted after
deformation and are now exposed in approximately cross-sectional view,
At high stratigraphic levels, deformation produced a slaty cleavage a
nd relatively open folds, both of which are concentrated in rheologica
lly incompetent rock types, and was accompanied by metamorphism at low
grade. At deeper stratigraphic levels, the regional foliation intensi
fies and becomes more pervasive, folds tighten, and metamorphic grade
increases through greenschist into amphibolite grade. At the deepest s
tratigraphic levels, the rocks are amphibolite grade L-S tectonites wi
th a pronounced mylonitic fabric. The similar to 2 km-thick-zone of my
lonites is interpreted as a ductile shear zone that formed when the st
ratigraphic section was still upright, whereas the less deformed, youn
ger rocks are interpreted to occupy the upper plate of the shear zone
and to record a strain gradient away from the shear zone. A variety of
structural and regional relations indicate that the shear zone is a d
uctile thrust fault along which younger rocks moved to the northwest (
in present-day coordinates) with respect to older rocks. The timing of
regional Jurassic deformation and metamorphism is constrained by rela
tions in and around two plutons dated by the U-Pb zircon method. The 2
01+/-1 Ma Big Creek pluton was intruded as a sill-like body along the
upper levels of the shear zone and is associated with a variety of fea
tures indicating syntectonic intrusion, including internal textural fe
atures in plutonic rocks and metamorphic changes in wall rocks with pr
oximity to the pluton. The 185+/-1 Ma Theodore pluton which intrudes a
cross part of the shear zone has a thermal aureole which statically ov
erprints the shear zone fabric. Deformation was thus ongoing at 201 Ma
and over by 185 Ma. The Early Jurassic age of regional shortening def
ormation in the Pine Forest Range contrasts with the Middle to Late Ju
rassic (similar to 170 similar to 150 Ma) age of regional shortening d
ocumented in many other parts of the Mesozoic are system, including th
e Klamath Mountains, Sierra Nevada, and Mojave Desert regions of Calif
ornia. It also contrasts with the record of Early Jurassic extensional
tectonism documented in the Sierra Nevada, Mojave Desert, and western
Arizona segments of the Mesozoic are system. These conflicting relati
ons indicate a complex tectonic evolution for the Jurassic U.S. Cordil
lera plate margin and lend support to the idea that disparate parts of
this plate margin were juxtaposed along younger strike-slip faults.