The tectono-stratigraphic evolution of distal, hyper-extended magma-poor conjugate rifted margins: Examples from the Alpine Tethys and Newfoundland–Iberia

Author:

Decarlis A.,Manatschal G.,Haupert I.,Masini E.

Funder

MM3 Consortium

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

Reference134 articles.

1. Petrochemistry of serpentinized peridotite from the Iberia Abyssal Plain (ODP Leg 173): its character intermediate between suboceanic and sub-continental upper mantle;Abe,2001

2. Mesozoic-Cenozoic evolution of North Atlantic continental-slope basins: the Peniche basin, western Iberian margin;Alves;AAPG Bull.,2006

3. Diachronous evolution of late Jurassic-cretaceous continental rifting in the northeast Atlantic (west Iberian margin);Alves;Tectonics,2009

4. Carta Geologica d'Italia alla scala 1:50000;Apat Servizio Geologico d'Italia,2008

5. A fossil, serpentinization-related hydrothermal vent, Ocean Drilling Program Leg 173, Site 1068 (Iberia Abyssal Plain): some aspects of mineral and fluid chemistry;Beard;J. Geophys. Res.,2000

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