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(Article of periodic en Anglais - 1982)

Document title

Plate motion may be measured in situ as subsidence at trenches

Authors(s) and Affiliation(s)

NAKAMURA K. ;

Abstract

The motion of the oceanic plates may be directly measured at trenches as the subsidence and possibly tilting rate though the intraplate deformations may affect the measure of long distances. A case is introduced where a part of the downgoing plate is emerged above sea-level in the Izu peninsula near the trench axis.

Source

Article of periodic

published at : Journal of the Geodetic Society of Japan Tokyo

Editor :

Millesime : 1982, vol. 28, no3 [pp. 174-176]

Bibliographic references : 13 réf.

Language

Anglais

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