Volume : 2, Issue : 5, MAY 2016

NEOTECTONIC ACTIVITY IN KACHCHH RIFT BASIN, WESTERN INDIA: EVIDENCED BY GEOMORPHIC MARKER AND PALEOSEISMIC FEATURES

Gaurav Chauhan, M. G. Thakkar, Girish Ch. Kothyari, Siddharth Prizomwala, Subhash Bhandari, S. K. Biswas

Abstract

Kachchh, a pericratonic rift basin, in Western India displays fault-controlled first-order topography. The five denudational cyclic surfaces identified indicate major episodes of tectonic movements responsible for evolution of the present landscape. The rift basin is defined by E-W trending master faults which bound the tilted upthrown blocks. A transverse fault system cuts across the E-W structural fabric. Geomorphic highs related to domes, anticlines, intrusive bodies and fault scarps associated with these faults suggest their active nature. The most striking feature of the basin is a NE-SW trending first order basement high or ridge across the master faults. This central high defined as Median High (MH) is active since Mid-Jurassic and plays a major role in the geomorphic evolution of the area. Present research highlights development of geomorphic signatures associated with neotectonic activity along master faults. The various tectono-geomorphic features confirms the basin is tectonically active in Quaternary period

Keywords

Geomorphic Marker, Rift, Median High, Master fault, half-graben.

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