Paleomagnetism of middle Miocene volcanic rocks in the Mojave-Sonora desert region of western Arizona and southeastern California

Journal Article · Wed Jan 10 00:00:00 EST 1990 · Journal of Geophysical Research; (United States)

DOI:https://doi.org/10.1029/JB095iB01p00625· OSTI ID:5010223

Calderone, G J ^[1]; Butler, R F; Acton, G D ^[2]

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1. Geological Survey, Flagstaff, AZ (United States)
2. Univ. of Arizona, Tucson (United States)

Paleomagnetic directions have been obtained from 190 early to middle Miocene (12-20 Ma) mafic volcanic flows in 16 mountain ranges in the Mojave-Sonora desert region of western Arizona and southeastern California. These flows generally postdate early Miocene tectonic deformation accommodated by low-angle normal faults but predate high-angle normal faulting in the region. After detailed demagnetization experiments, 179 flows yielded characteristic directions interpreted as original thermal remanent magnetizations (TRM). Because of the episodic nature of basaltic volcanism in this region, the 179 flows yielded only 65 time-distinct virtual geomagnetic poles (VGPs). The paleomagnetic pole calculated from the 65 cooling unit VGPs is located at 85.5{degree}N, 108.9{degree}E within a 4.4{degree} circle of 95% confidence. This pole is statistically indistinguishable (at 95% confidence) from reference poles calculated from rocks of similar age in stable North America and from a paleomagnetic pole calculated from rocks of similar age in Baja California. The coincidence of paleomagnetic poles from the Mojave-Sonora desert region with reference poles from the stable continental interior indicates that (1) significant vertical axis net tectonic rotations have not accompanied post-middle Miocene high-angle normal faulting in this region; (2) there has been no detectable post-middle Miocene latitudinal transport of the region; and (3) long-term nondipole components of the middle Miocene geomagnetic field probably were no larger than those of the recent (0-5 Ma) geomagnetic field. In contrast, paleomagnetic data indicate vertical axis rotations of similar age rocks in the Transverse Ranges, the Eastern Transverse Ranges, and the Mojave Block.

• OSTI ID: 5010223
• Journal Information: Journal of Geophysical Research; (United States), Vol. 95:B1; ISSN 0148-0227
• Country of Publication: United States
• Language: English

Related Subjects

58 GEOSCIENCES
ARIZONA
GEOLOGIC FORMATIONS
CALIFORNIA
PALEOMAGNETISM
AGE ESTIMATION
DEFORMATION
DESERTS
GEOLOGIC FAULTS
GEOLOGIC HISTORY
GEOMAGNETIC COORDINATES
GEOMAGNETIC FIELD
MAGNETIZATION
MIOCENE EPOCH
MOUNTAINS
ROTATION
TECTONICS
VOLCANIC ROCKS
VOLCANISM
ARID LANDS
CENOZOIC ERA
COORDINATES
DEVELOPED COUNTRIES
FEDERAL REGION IX
GEOLOGIC AGES
GEOLOGIC FRACTURES
GEOLOGIC STRUCTURES
IGNEOUS ROCKS
MAGNETIC FIELDS
MAGNETISM
MOTION
NORTH AMERICA
ROCKS
TERTIARY PERIOD
USA
580000* - Geosciences