Abstract
The term “rift” was introduced, in 1896, by Gregory for a structural graben in Africa (now the Gregory Rift), then for the entire continental system of grabens of which this was a part (the East African Rift system). Since then, until the onset of plate tectonics in 1968, “riftology” became an established branch of geotectonics and a fairly mature one in terms of global inventarization and description of the visually discernible (i.e. mostly geologically young) physiographic rifts. Since 1968 “riftology” has continued its evolution as an integral part of the New Global Tectonics.
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Laznicka, P. (2010). Rifts, paleorifts, rifted margins, anorogenic and alkaline magmatism. In: Giant Metallic Deposits. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-12405-1_12
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