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Late Pleistocene-Holocene uplift driven terrace formation and climate-tectonic interplay from a seismically active intraplate setting: An example from Kachchh, Western India
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文摘

The study uses detailed sedimentology, OSL chronology and palaeo-monsoonal proxies.

Terrace formation is chiefly regulated by uplifts in tectonically active regions.

Dryland response to Early Holocene Optima and the Younger Dryas was investigated.

Three pulsative uplifts along KMF are recorded with a minimum uplift rate of 1.04 mm/a.

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