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      Seismic slip propagation to the updip end of plate boundary subduction interface faults: Vitrinite reflectance geothermometry on Integrated Ocean Drilling Program NanTro SEIZE cores

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          The energy release in great earthquakes

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            Source mechanisms and tectonic significance of historical earthquakes along the nankai trough, Japan

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              Splay Fault Branching Along the Nankai Subduction Zone

              J.-O. Park (2002)
              Seismic reflection profiles reveal steeply landward-dipping splay faults in the rupture area of the magnitude (M) 8.1 Tonankai earthquake in the Nankai subduction zone. These splay faults branch upward from the plate-boundary interface (that is, the subduction zone) at a depth of approximately 10 kilometers, approximately 50 to 55 kilometers landward of the trough axis, breaking through the upper crustal plate. Slip on the active splay fault may be an important mechanism that accommodates the elastic strain caused by relative plate motion.
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                Author and article information

                Journal
                Geology
                Geology
                Geological Society of America
                0091-7613
                1943-2682
                March 17 2011
                March 08 2011
                : 39
                : 4
                : 395-398
                Article
                10.1130/G31642.1
                c7fe7139-0fcb-497b-bc90-f58cb8cb4f11
                © 2011
                History

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