Deformation and exhumation at convergent margins

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