Abstract
A normal oceanic crust cannot be generated after continental crust splitting of rifts filled by a thick pile of young sediments. The magma released by the rising mantle is trapped mainly in these sediments as basalts sills and plugs. The sediments are themselves metamorphosed by the heat flux from the underlying mantle. A metasedimentary crust is formed in direct contact with an abnormal mantle (Vp ā 7.5 km sāl) produced by partial serpentinization.
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Nicolas, A. Novel type of crust produced during continental rifting. Nature 315, 112ā115 (1985). https://doi.org/10.1038/315112a0
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DOI: https://doi.org/10.1038/315112a0
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