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En echelon Miocene rifting in the southwestern United States and model for vertical-axis rotation in continental extension

Journal Article · · Geology; (United States)
 [1];  [2]
  1. Univ. of Utah, Salt Lake City (United States)
  2. Univ. of North Carolina, Chapel Hill (United States)
Two areas of intense early Miocene crustal extension in the southwestern United States, the Colorado River trough and the central Mojave Desert, are separated by a weakly deformed area in the eastern Mojave Desert. The authors propose that these areas form a left-stepping en echelon rift system linked by a ductile detachment at depth. The en echelon geometry explains the southward loss of displacement in the central Mojave Desert and northward loss of coeval displacement in the Colorado River trough, and it incorporates seismic reflection evidence that mid-crustal Tertiary extensional mylonites continue beneath the weakly deformed area. This geometry also explains clockwise paleomagnetic declination anomalies from lower Miocene rocks as recording thin-skinned, detached rotations; large-scale block rotations are not required. Obliquity of the northeast-trending crustal-extension vector to the east-west-trending early Miocene synextensional volcanic belt may have caused the en echelon pattern to develop.
OSTI ID:
7201985
Journal Information:
Geology; (United States), Journal Name: Geology; (United States) Vol. 19:12; ISSN GLGYB; ISSN 0091-7613
Country of Publication:
United States
Language:
English