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Inherited structures and lateral variability along a plate boundary shear zone in a convergent margin: The Sestola-Vidiciatico Tectonic Unit and the Subligurian Units of the Northern Apennines of Italy
No full textCurettage of giant cell tumor of bone. The effect of surgical technique and adjuvants on local recurrence rate
No full textCurettage of giant cell tumor of bone. The effect of surgical technique and adjuvants on local recurrence rate
Assenza di complicanze cardiache nei pazienti portatori di turbe intraventricolari della conduzione sottoposti ad anestesia per intervento chirurgico.
No full textAssenza di complicanze cardiache nei pazienti portatori di turbe intraventricolari della conduzione sottoposti ad anestesia per intervento chirurgico
[The Rizzoli Orthopedic Institute modular-type prosthesis for the proximal femur; preliminary results]
No full textCurettage of giant cell tumor of bone. Reconstruction with subchondral grafts and cement
No full textCurettage of giant cell tumor of bone. Reconstruction with subchondral grafts and cement
Fluid history related to the early Eocene-middle Miocene convergent system of the Northern Apennines (Italy). Constraints from structural and isotopic studies
Full text linkThe late Eocene-middle Miocene erosive plate boundary between the European and
the Adriatic plates is exhumed in the Northem Apennines of Italy. The fossil fault zone is
500 m thick and the outcropping portion exposes the :first 5 km of its depth. At this
plate boundary basai and frontal tectonic erosion incorporated unlithified, fluid-rich sediments
into the fault zone. The deformation and nature of the material along the plate boundary define a
fossil subduction channel. Here we couple a detailed structural analysis of the Apennine subduction
channel, focusing, in particular, on calcite veins, with a stable isotope analysis to characterize
the fluid regime along an active subduction channel.
The 13C and 180 composition of calcite vein and host rock samples within the fault zone
indicates that there is a deep metamorphic source of fluids migrating upward along the subduction
channel, in addition to locally derived fluid components. Dewatering of subducting turbidites
contributes significantly only in the shallowest part of the channel. Structural observations
indicate fluid flow along and across the subduction channel. At deep levels fluid flow is
associated with discrete deformation events on shear faults offset by dilational jogs :filled with
implosion breccias. At intennediate levels deformation is stili cyclic and associated with repeated
crack-and-seal events. At the shallowest levels deformation occurred, while portions of the
subducting material were stili unlithi:fied. Here the deformation was quasicontinuous, without
associated vein development. Both isotope and structural analyses indicate that this erosive
subduction channel behaved as a weak: fault with a vertical maximum principal stres
Curettage of giant cell tumor of bone. Introduction - material and methods
No full textCurettage of giant cell tumor of bone. Introduction - material and methods
"Trattamento con Perle di Cemento alla Gentamicina di Infezioni dopo Interventi per Tumori Ossei"
No full text"Trattamento con Perle di Cemento alla Gentamicina di Infezioni dopo Interventi per Tumori Ossei
Functional results of prosthetic knee replacement after resection of the distal femur
No full textFunctional results of prosthetic knee replacement after resection of the distal femur
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