, Jacques Déverchère & R.W. Ferdinand
Understanding the forces that initiate continental break-up needs to find sites where magmatism and rifting interact. The thermal structure of the mantle and the crust, the products of partial melting, the position(s) and nature(s) of the inherited structures (cratonic blocks, old lithospheric sutures) play a key role on earthquake genesis and have to be studied into details using different, multi-scale, approaches. The North Tanzanian Divergence (NTD) is one of the unique areas in the world...
4 citations reported since publication in 2007.
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