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

Figure 10

Distribution of hydrothermal manifestations in the Lhasa block of the Tibetan plateau (about 80–94°E, 27–33°N). 1: Early major compressive or compressive-shear fault: the upper one is the Bangong-Nujiang suture zone, and the lower one is the Yarlung Zangbo Jiang suture zone; 2: the number of active tectonic zone; 3: boundary fault in active tectonic zone; 4: faulted-depression zone in active tectonic zone; 5: site of sampling; 6: boiling spring; 7: hydrothermal explosion, geyser and boiling fountain; 8: thermal spring; 9: hot spring; 10: untested hydrothermal area (according to [21]).