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Geodetic strain in peninsular Italy between 1875 and 2001

Abstract:

We determine geodetic strain in peninsular Italy by the GPS reoccupation of the first order triangulation network of Italy installed from 1860. The uncertainties in the original measurements (about 3 ppm), and the time span between the two observations, imply that tectonic signals larger than about 0.03 ppm/yr are resolvable. Along the Apenninic belt, where the largest earthquakes are concentrated, the geodetic deformation has a clear and consistent strain pattern between adjacent regions, we...

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Publication status:
Published

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Publisher copy:
10.1029/2002GL016447

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Journal:
GEOPHYSICAL RESEARCH LETTERS
Volume:
30
Issue:
4
Pages:
30-1
Publication date:
2003-02-25
DOI:
ISSN:
0094-8276
Language:
English
Pubs id:
pubs:178190
UUID:
uuid:a75f3397-45b2-45fa-a50b-762f3fe35317
Local pid:
pubs:178190
Source identifiers:
178190
Deposit date:
2012-12-19

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