Cenozoic Geology of Southwestern High Plateaus of Utah 1-1-001-320-4330-320 quantification of strain in folds

quantification of strain in folds at the tips of dextral faults

Five of the papers are on sequence stratigraphy and related topics (ranging from the Ordovician through the Devonian)

Tectonic Evolution

Editors: Manuel Sintubin

Cenozoic Geology of Southwestern High Plateaus of Utah 1-1-001-320-4330-320 quantification of strain in foldsAuthors: John J. Anderson, Peter D. Rowley, Robert J. Fleck, and A. E. M. Nairn The southwestern High Plateaus of Utah and an adjacent portion of the Great Basin were the site of extensive and prolonged volcanism during much of the Cenozoic Era. The volcanic pile that is centered near Marysvale, Utah, consists mostly of intermediate lava flows and volcanic breccia and dominates the vast accumulation of eruptive deposits that blankets this region; this