TECTONIC ROTATIONS WITHIN THE RIO-GRANDE RIFT - EVIDENCE FROM PALEOMAGNETIC STUDIES

Paleomagnetic studies on Miocene-Pliocene volcanic rocks from the Espanola basin of the Rio Grande rift, New Mexico, reveal directions discordant from the expected mean direction for North America. The Paliza Canyon Formation, Tschicoma Formation, and Lobato Basalt, all sampled in the Jemez Mountains west of the Pajarito fault zone, have mean declinations east of the expected mean. The Cerros del Rio volcanics, lying east of the Pajarito fault zone, have a westerly declination. Combined with published data on the Santa Fe Group sediments east of the fault zone, and the Valles Rhyolite, west of the fault zone, distinct rotations of the two areas are evident. The western block has rotated clockwise 12 degree , while the eastern block shows 16 degree of counter-clockwise motion. Differential rotations of 25 degree -30 degree are calculatd between the two blocks; 4 degree /m. y. is the minimum differential rotation for the past 5 m. y.