Results 221 to 230 of about 15,237 (275)

Ivrea mantle wedge, arc of the Western Alps, and kinematic evolution of the Alps–Apennines orogenic system [PDF]

open access: yesSwiss Journal of Geosciences, 2017
The construction of five crustal-scale profiles across the Western Alps and the Ivrea mantle wedge integrates up-to-date geological and geophysical information and reveals important along strike changes in the overall structure of the crust of the ...
Tobias Diehl   +2 more
exaly   +5 more sources

Receiver function mapping of the mantle transition zone beneath the Western Alps: New constraints on slab subduction and mantle upwelling [PDF]

open access: yesEarth and Planetary Science Letters, 2022
International audienceTo better constrain the deep structure and dynamics of the Western Alps, we studied the mantle transition zone (MTZ) structure using P-wave receiver functions (RFs). We obtained a total of 24904 RFs from 1182 events collected by 307
Elena Eva, Marco Giovanni Malusa
exaly   +2 more sources
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Thickening history of the Western Alps

Earth and Planetary Science Letters, 1986
A model of evolution for the western segment of the Alpine chain is presented. Available data concerning the structural, metamorphic and geochronological evolution in the majorunits involved in the thickening processes are takeninto account IO constrain the model.
Ph. Gillet   +3 more
openaire   +1 more source

New occurrence of deerite in the Western Alps

1978
Deerite has been found in the Cu-Fe sulfide deposit of Viafiorcia, Western Alps, associated with the Piemonte ophiolite nappe. This hydrous, ferrous, ferric silicate occurs together with Na-amphibole, stilpnomelane+/- white mica, albite and carbonate, and with pyrite, chalcopyrite, bornite, pyrrothite, magnetite +/- sphalerite, mackinawite, linneite ...
DAL PIAZ G. V., MOLIN, GIANMARIO
openaire   +2 more sources

Episodic exhumation in the Western Alps

Geology, 2003
Oligocene to Miocene clastic sediments of the Tertiary Piedmont Basin (northwest Italy) were derived from erosion of Western Alps source rocks. Detrital white micas from dif- ferent stratigraphic units and from sands of three present-day rivers draining the internal Western Alps have been analyzed by 40 Ar/ 39 Ar geochronology. Our data suggest a wide-
Barbara Carrapa   +2 more
openaire   +1 more source

The western alps: Palaeogeography and structure

Earth-Science Reviews, 1970
Abstract Presented is a short review of main palaeographic and tectonic features of the Western Alps, with numerous references to recent works, mainly those later than 1950.
J. Debelmas, M. Lemoine
openaire   +1 more source

Collision tectonics in the Western Alps

Geological Society, London, Special Publications, 1986
Summary This paper gives a brief review of some different models that have been proposed to account for the tectonic development of the Western Alps, emphasizing the field evidence which indicates the major role played by strike-slip tectonics. Sketch maps of the tectonic evolution since Cretaceous times are presented which interpret the Alps
L. E. Ricou, A. W. B. Siddans
openaire   +1 more source

Interplay between erosion and tectonics in the Western Alps

Terra Nova, 2006
AbstractBedrock fission‐track analysis, high‐resolution petrography and heavy mineral analyses of sediments are used to investigate the relationships between erosion and tectonics in the Western Alps. Along the Aosta Valley cross‐section, exhumation rates based on fission‐track data are higher in the fault‐bounded western block than in the eastern ...
MALUSA', MARCO GIOVANNI   +1 more
openaire   +2 more sources

France and The Western Alps

2014
The use of copper was first established in the western Alps during the late fifth/ early fourth millennia BC. There were several metal-using groups in what is now modern Switzerland during the fourth millennium, including the Cortaillod and Pfyn cultures, followed in the third millennium BC by groups of the Saône-Rhône culture (Strahm 1994).
openaire   +1 more source

A multidisciplinary approach to the study of the fault networkin the internal Cottian Alps (Western Alps)

Italian Journal of Geosciences, 2009
The architecture of the fault network and the late- to post-metamorphic structural evolution in the internal Cottian Alps have been studied by an integrated approach combining morphostructural analysis, field mapping and detailed mesostructural analysis between the Susa and Pellice Valleys. Available apatite fission track data indicate that this sector
Perrone Gianluigi   +4 more
openaire   +3 more sources

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