Informatics Publishing Limited

Javed N. Malik ¹, Michio Mornio ², Prashant Mishra ¹, Chandrashekar Bhuiyan ¹, Fumio Kaneko ²

Affiliations
1 Department of Civil Engineering, Indian lnstltute of Technology Kanpur, Kanpur-208016, IN
2 OYO International Corporation, Rokubancho Kyodo Bldg 2F, 6 Rokubancho, Chiyoda-ku, Tokyo-102-0085, JP

Abstract

We report first ldentified active fault exposure from Kachchh region along the Kachchh Mainland Fault (KMF) other than the 1819 Allah Bund earthquake. The active fault scarps striking E-W were identified near Lodai vlilage along KMF North facing scarps with height from 10-15 m are the manifestation of the displaced alluvial fan surface along this fault. Occurrence of discontinuous linear mound ranging in height from 3-5 m aligned along the strike about 100 m north of the main scarp are suggestive of younger tectonic movement and progressive shift of tectonic activity towards north along new imbricated fault. Three low to high angle reverse fault strands (F₁, F₂ and F₃) displacing young Quaternary deposits (late Pleistocene-Holocene?) classified as A to F unlts comprising gravel and sand-Silt facies were identifled in a trench excavated at the base of the linear mound along KMF. Our preliminary observations revealed occurrence of atleast two large magnitude earthquakes along the F₃ fault, and may be older events along the F₁ and F₂. Latest event (Event-I) occurred along F₃ after the deposition of unit B registering the displacement of -33 cm, penultimate event (Event-11) occurred after the deposition of unit C with -40 cm of displacement. The maximum displacement of about 73 cm along F₃ indicates cumulative displacement accommodated during more than one event. The total displacement of -98 cm along F₂ strand displacing the E and F units is the result of more than one event, and since the F₂ probably displaced the unit C suggests that the movements occurred during penultimate (Event 11) and during the Event 111, older than penultimate. Displacement of Mesozoic succession during older events and unit B during the latest Event I along F₁ suggests repetitive movement along this fault. The fragile nature of -3-4 m wide shear zone formed in Mesozoic rocks (shale+sandstone) also point towards repetitive tectonic movement along KMF.

Keywords

Active Fault, Paleoseismic investigation, paleo-Earthquakes, Kachchh Mainland fault, Kachchh, Gujarat.

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