Abstract
The rift regime is similar to the orogenic and is sometimes considered a variety of the latter. A number of specific features, however, lead us to classify it in an autonomous category.
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© 1980 English translation, Mir Publishers
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Beloussov, V.V. (1980). Rift, Magmatic Activization, and Continental Margin Regimes. In: Geotectonics. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-67176-0_17
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DOI: https://doi.org/10.1007/978-3-642-67176-0_17
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-67178-4
Online ISBN: 978-3-642-67176-0
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