Title: Deformation and exhumation at convergent margins
First published: 2008
Description: "The Franciscan subduction complex formed a long-lived accretionary wedge of Late Jurassic through Oligocene age that fringed the western edge of the North American Cordillera. This volume summarizes absolute finite-strain data from the Franciscan subduction complex and brittle strain data from important faults in and above this complex. Because the Franciscan is generally considered a prototypical sediment-rich subduction complex, its tectonic evolution is important for understanding convergent plate margins, and the results outlined in this volume may have broad implications for other subduction-zone settings."--Pub. desc.
Subjects: Convergent margins, Franciscan Complex (Calif.), Geology, Structural, Plate tectonics, Structural Geology, Subduction zones
Places: Northern California
LC classification: QE627.5.C2 R56 2008