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Northern Potwar Deformed Zone (NPDZ) is a part of the foreland zone of NW Himalayan folds and thrust belt. Seismicity map has been prepared for this region, which appears to be less active as compared with adjacent regions with apparently no distinct pattern or relationship with surface structures. Focal mechanism solutions of 4 events, for which required parameters are available, indicate left-lateral strike-slip faulting for 3 events and thrusting for one event. P-axes orientations are in NW-SE and NE-SW. Basement is most likely involved in the ongoing deformation.

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The conference comprised four-days of indoor oral and poster presentations and two post-conference field excursions to the Emeishan large igneous province and the North China Craton.The conference attracted over 200 scientists (including 53 graduate students) from 28 countries including Australia,