Extensional Seismogenic Stress and Tectonic Movement on the Central Region of the Tibetan Plateau

<table>Distribution of the fault plane solutions for the normal-fault-type events (1933-2003, <svg height="11.85" id="M3" style="vertical-align:-0.546pt" version="1.1" viewbox="0 0 42.849998 11.85" width="42.849998" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink">
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h170v-28q-68 -6 -81 -21.5t-11 -91.5l9 -362q2 -80 15 -97t78 -22v-28z" id="x4D"></path></g><g transform="matrix(.017,-0,0,-.017,19.917,11.113)"><path d="M531 285l-474 -214v56l416 183l-416 184v56l474 -215v-50zM531 -40h-474v50h474v-50z" id="x2265"></path></g><g transform="matrix(.017,-0,0,-.017,34.621,11.113)"><path d="M153 550l-26 -186q79 31 111 31q90 0 141.5 -51t51.5 -119q0 -93 -89 -166q-85 -69 -173 -71q-32 0 -61.5 11.5t-41.5 23.5q-18 17 -17 34q2 16 22 33q14 9 26 -1q61 -50 124 -50q60 0 93 43.5t33 104.5q0 69 -41.5 110t-121.5 41q-53 0 -102 -20l38 305h286l6 -8
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</svg>) in and around the Tibetan plateau.</table>

International Journal of Geophysics

fig8

Figure 8

Figure 8: Extensional Seismogenic Stress and Tectonic Movement on the Central Region of the Tibetan Plateau 