Results 61 to 70 of about 217 (106)

An update of Jurassic ophiolites and associated calc-alkaline rocks in the South Apuseni Mountains (Western Romania). [PDF]

open access: yes, 2004
Bortolotti, Valerio   +5 more
core  

The preorogenic tectonic history of the Bracco gabbroic massif: review and news [PDF]

open access: yes, 2007
Corti, S.   +4 more
core  
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Evoluzione tettono-sedimentaria del Complesso d’Accrezione Liguride in Appennino Meridionale

Rendiconti Online della Società Geologica Italiana, 2013
Tectono-sedimentary evolution of the Ligurian Accretionary Complex in the southern Apennines.Aim of this paper is the structural and stratigraphic analyses of the Ligurian Accretionary Complex exposed in the Campania region (Italy) in order to unraveling the deformation pattern characterizing the transition from the final oceanic subduction stages to ...
VITALE, STEFANO   +5 more
openaire   +2 more sources

The Liguride Complex of Southern Italy —a Cretaceous to Paleogene accretionary wedge

Tectonophysics, 1987
Abstract The ophiolite-bearing allochthonous flysch (Liguride Complex) of the Southern Apennines, Italy, has traditionally been divided into two tectonic units: the metamorphic Frido Unit and the unmetamorphosed Cilento Unit. The two units have hitherto been considered to derive from two distinct paleogeographic domains; however, the identification ...
INVERNIZZI C   +5 more
openaire   +7 more sources

Isotopic contrasts within the Internal Liguride ophiolite (N. Italy): the lack of a genetic mantle–crust link

Earth and Planetary Science Letters, 1998
It is widely accepted that oceanic lithosphere is generated by partial melting of fertile mantle peridotites producing basaltic melts and residual peridotites. This theory implies a cogenetic relationship between peridotites and associated crustal rocks, but the actual existence of such a genetic link has been tested in very few places.
RAMPONE, ELISABETTA   +2 more
openaire   +3 more sources

Structure, kinematics and metamorphism in the Liguride Complex, southern Apennines, Italy

Journal of Structural Geology, 1994
Abstract The Liguride Complex of south Italy is the remains of a Cretaceous-Paleogene accretionary wedge which was emplaced onto the African margin during Early Miocene time. Transport directions of thrust sheets and nappes in the internal zone are roughly towards the present-day northeast.
openaire   +1 more source

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