عنوان
پدید آورنده
موضوع
رده
کتابخانه
محل استقرار
0813724457
9780813724454
b523341
Deformation and exhumation at convergent margins :
[Book]
the Franciscan subduction complex /
Uwe Ring
Boulder, Colo. :
Geological Society of America,
[2008]
©2008
0810
v, 61 pages :
illustrations, maps ;
28 cm
Special papers (Geological Society of America) ;
445
Includes bibliographical references
The Franciscan triad -- an overview -- Pressure-temperature evolution and evidence for solution-mass-transfer deformation -- Methods of strain analysis, sampling, and data collection -- Brittle strain on the coast range fault zone -- Brittle strain in the Franciscan subduction complex Ductile strain and mass loss in the eastern and central franciscan belts -- Role of ductile thinning of the overburden to exhumation of the high-pressure metamorphic rocks
0
"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
Convergent margins-- California, Northern
Geology, Structural-- California, Northern
Plate tectonics-- California, Northern
Subduction zones-- California, Northern
Franciscan Complex (Calif.)
0
Ring, Uwe
20090116115453.0
rda
مطالعه متن کتاب [Book]
Y
