Recognizing remnants of magma-poor rifted margins in high-pressure orogenic belts: The Alpine case study

Magma-poor rifted margins are being increasingly recognized in present-day Atlantic-type systems. However, findings of fossil areas floored by exhumed mantle or hyper-extended crust are comparatively rare within orogenic belts that were originated through the inversion of pre-existing rifted margins...

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Veröffentlicht in:	Earth-science reviews 2014-04, Vol.131, p.88-115
Hauptverfasser:	Beltrando, Marco, Manatschal, Gianreto, Mohn, Geoffroy, Dal Piaz, Giorgio Vittorio, Vitale Brovarone, Alberto, Masini, Emmanuel
Format:	Artikel
Sprache:	eng
Schlagworte:	Alps Convergent margin dynamics Extensional allochthons Hyper-extended crust Igneous rocks Life Sciences Lithology Magma Mapping Rift inheritance Rock deformation Sedimentation & deposition Stratigraphy
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