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Measurement of interseismic strain accumulation across the North Anatolian Fault by satellite radar interferometry

Abstract:

In recent years, interseismic crustal velocities and strains have been determined for a number of tectonically active areas through repeated measurements using the Global Positioning System. The terrain in such areas is often remote and difficult, and the density of GPS measurements relatively sparse. In principle, satellite radar interferometry can be used to make millimetric-precision measurements of surface displacement over large surface areas. In practice, the small crustal deformation s...

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Publication status:
Published

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Publisher copy:
10.1029/2000GL012850

Authors


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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
Journal:
GEOPHYSICAL RESEARCH LETTERS More from this journal
Volume:
28
Issue:
10
Pages:
2117-2120
Publication date:
2001-05-15
DOI:
ISSN:
0094-8276
Language:
English
Pubs id:
pubs:82169
UUID:
uuid:fb4edda9-54ed-4311-9fa1-fe12bee8bb09
Local pid:
pubs:82169
Source identifiers:
82169
Deposit date:
2012-12-19

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