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The importance of microearthquakes in crustal extension of an active rift: A case study from New Zealand

Author
MOUSLOPOULOU, Vasiliki1 2 ; HRISTOPULOS, Dionissios T1 ; NICOL, Andrew3 ; WALSH, John J4 ; BANNISTER, Stephen3
[1] Department of Mineral Resources Engineering, Technical University of Crete, Chania, Greece
[2] Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Telegrafenberg, Potsdam, Germany
[3] GNS Science, Lower Hutt, New Zealand
[4] Fault Analysis Group, School of Geological Sciences, University College Dublin, Dublin, Ireland
Source

Journal of geophysical research. Solid earth. 2013, Vol 118, Num 4, pp 1556-1568, 13 p ; ref : 1 p

ISSNNV
2169-9313
Scientific domain
Astronomy earth cosmic environment; Geology; Geophysics; Climatology, meteorology; Oceanography
Publisher
Wiley, Hoboken, NJ
Publication country
United States
Document type
Article
Language
English
Keyword (fr)
Déformation sous contrainte Déplacement Ecart type Etude cas Extension Magnitude Microséisme Microtremblement de terre Profondeur Qualité Rift Rupture Système GPS Séisme Nouvelle Zélande Australasie
Keyword (en)
strain displacements standard deviation case studies extension magnitude microseisms microearthquakes depth quality rift zones rupture Global Positioning System earthquakes New Zealand Australasia
Keyword (es)
Deformación bajo tensión Desviación típica Estudio caso Extensión Magnitud Microsismo Microsacudida Profundidad Calidad Rift Ruptura Sismo Nueva Zelandia Australasia
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
27667749

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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