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PRELIMINARY OBSERVATIONS FROM A TRENCH NEAR CHANDIGARH, NW HIMALAYA AND THEIR BEARING ON ACTIVE FAULTING (2003)
Evidence of two parallel to sub-parallel active-fault traces along the Himalayan Front around Chandigarh has provided additional information on the imbricated faulting pattern that branches out from the Himalayan Frontal Thrust system, which probably merges down northward with dcollement. In this paper are presented some preliminary paleoseismic observations from trench excavated near Chandigarh
Reference:
CURRENT SCIENCE, VOL. 85, NO. 12, 25 DECEMBER 2003
CURRENT SCIENCE, VOL. 85, NO. 12, 25 DECEMBER 2003
Organization:
Department of Civil Engineering, Indian Institute of Technology, Kanpur 208 016, India
India, Himalaya
Department of Civil Engineering, Indian Institute of Technology, Kanpur 208 016, India
India, Himalaya
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