The southern Tyrrhenian subduction zone: Deep geometry, magmatism and Plio-Pleistocene evolution-Reference-Cited by-同舟云学术

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The southern Tyrrhenian subduction zone: Deep geometry, magmatism and Plio-Pleistocene evolution

Published:2008-04 Issue:3-4 Volume:268 Page:408-423
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Chiarabba Claudio,De Gori Pasquale,Speranza Fabio

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference74 articles.

1. Hydrated subducted crust at 100–250 km depth;Abers;Earth Planet. Sci. Lett.,2000

2. The thermal structure of subduction zones constrained by seismic imaging: implications for slab dehydration and wedge flow;Abers;Earth Planet. Sci. Lett.,2006

3. Fragmentation of the Alpine orogenic belt by microplate dispersal;Alvarez;Nature,1974

4. Non-linear global P-wave tomography by iterated linearized inversion;Bijward;Geophys. J. Int.,2000

5. Plio-Quaternary megasequence geometry and its tectonic controls within the Maghrebian thrust belt of south-central Sicily;Butler;Terra Nova,1995

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