Jurassic Magmatism and Tectonics of the North American Cordillera

Structural and stratigraphic development of the Middle Jurassic magmatic arc in the Cowhole Mountains, central-eastern Mojave Desert, California Available to Purchase
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Published:January 01, 1995
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CiteCitation
William B. Wadsworth, Horacio Ferriz, Dallas D. Rhodes, 1995. "Structural and stratigraphic development of the Middle Jurassic magmatic arc in the Cowhole Mountains, central-eastern Mojave Desert, California", Jurassic Magmatism and Tectonics of the North American Cordillera, David M. Miller, Cathy Busby
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The Cowhole Mountains, near Baker, California, are an east-tilted remnant of the Jurassic magmatic arc that extends from western Nevada through southeastern California into Arizona and Sonora, Mexico. In Middle Jurassic time, two northeast-erly trending grahens bounded by syndepositional faults accumulated 550 m and 700 m of predominantly eolian sandstone (Aztec Sandstone). Because east dip in one of the grabens increases from 30° at the base of the sandstone section to 65° at its top, we infer that structure to have developed during tilting to the west on east-dipping, listric normal faults. Westward tilting continued to accumulate during extrusion of an overlying Middle Jurassic volcanic series (Cowhole volcanics). Felsic volcanic rocks that buried the grabens comprise ignimbrites, volcaniclastic rocks, and flow breccias, emplaced in a proximal but extra-caldera setting. Plutons and sills were intruded at shallow levels, possibly during both graben filling and extrusion of volcanics. Local magmatism of significant volume ended with intrusion of a dike swarm that may be correlative with the Independence dike swarm (148 Ma). After the range tilted 90° toward the east, small glide blocks and landslides detached from high portions of the eroding range and descended into the southern graben.
Our model suggests that two sets of high-angle normal faults, oriented nearly at right angles to each other, were active during the same Middle Jurassic interval. A modern analogue may be provided by the Central American arc graben, in which similar transtensional structures have developed perpendicular to the regional graben where it is intersected obliquely by the Chiapas shear zone.
- Aztec Sandstone
- block structures
- breccia
- California
- carbonate rocks
- clastic rocks
- correlation
- dike swarms
- dip
- evolution
- faults
- felsic composition
- geologic maps
- grabens
- high-angle faults
- igneous activity
- igneous rocks
- ignimbrite
- intrusions
- Jurassic
- landslides
- lateral faults
- left-lateral faults
- listric faults
- maps
- mass movements
- Mesozoic
- Middle Jurassic
- models
- Mojave Desert
- normal faults
- orientation
- plutons
- pyroclastics
- sandstone
- sedimentary rocks
- sills
- stratigraphy
- structural geology
- systems
- tectonics
- thickness
- tilt
- transtension
- United States
- volcanic rocks
- volcaniclastics
- Baker California
- Cowhole Mountains
- Independence dike swarm
- Cowhole Volcanics
- Cowhole Fault
- Chiapas shear zone