Abstract
The occurrence of two large earthquakes (M>7.5) in the Kachchh basin within a short span of ∼200 years is quite unusual for an intracratonic region (Figure l). What factors could possibly make this region different from other, mid‐plate settings? Could some of these factors be responsible for the relatively shorter recurrence times? Does the tectonic history provide us with any clues about the uniqueness of this intraplate region?
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