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RECENT ADVANCES IN PERI-ADRIATIC GEODYNAMICS AND FUTURE RESEARCH DIRECTIONS Read chapter Read first chapter

2006 | OriginalPaper | Chapter

FRAGMENTATION OF ADRIA AND ACTIVE DECOLLEMENT TECTONICS WITHIN THE SOUTHERN PERI-TYRRHENIAN OROGEN, ITALY

Authors : John. S. Oldow, Luigi. Ferranti

Published in: The Adria Microplate: GPS Geodesy, Tectonics and Hazards

Publisher: Springer Netherlands

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Seismicity and GPS velocities in the southern peri-Tyrrhenian orogen record complex differential motion amongst crustal blocks constituting the tectonically fragmented paleotectonic domain, Adria. Coeval transpressional and transtensional belts within the orogen are kinematically coordinated and are consistent with displacement above a through-going basal decollement system that separates the heterogeneously deforming upper and middle crust from a presumed pattern of regular displacement within the underlying lithosphere. Seismicity and GPS velocities within the orogen reflect only indirectly the relative convergence between Africa and Eurasia.

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previous chapter ACTIVE DEFORMATION OF THE NORTHERN ADRIATIC REGION:Results from the CRODYN geodynamical experiment
next chapter GEODETIC MEASUREMENTS IN THE AEGEAN SEA REGION FOR THE DETECTION OF CRUSTAL DEFORMATION
Metadata
Title
FRAGMENTATION OF ADRIA AND ACTIVE DECOLLEMENT TECTONICS WITHIN THE SOUTHERN PERI-TYRRHENIAN OROGEN, ITALY
Authors
John. S. Oldow
Luigi. Ferranti
Copyright Year
2006
Publisher
Springer Netherlands
Book
The Adria Microplate: GPS Geodesy, Tectonics and Hazards

Print ISBN: 978-1-4020-4233-1

Electronic ISBN: 978-1-4020-4235-5

Copyright Year: 2006

DOI
https://doi.org/10.1007/1-4020-4235-3_19