DEEP-CRUSTAL SEISMOLOGY OF CONTINENTAL MARGINS

This review discusses results from recent seismic experiments at continental margins conducted by U.S. investigators as well as those by non‐U. S. investigators necessary to place the results of U.S. workers into context. Continental margins may be characterized as either rifted, transform, or convergent. Rifted (or passive) margins form where continents are torn apart during continental drift. Transform margins accommodate transform plate motions along strike‐slip faults such as the San Andreas fault. At convergent margins oceanic crust is being thrust beneath (or subducted under) the continental crust. All three types of margins are found in North America. Copyright 1995 by the American Geophysical Union.