Constraining fault growth rates and fault evolution in New Zealand

Understanding how faults propagate, grow and interact in fault systems is important because they are primarily responsible for the distribution of strain in the upper crust. They localise deformation and stress release, often producing surface displacements that control sedimentation and fluid flow...

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Bibliographic Details
Main Authors: Lamarche, G. (Author), Bull, J.M (Author), Barnes, P.M (Author), Taylor, S.K (Author), Horgan, H. (Author)
Format: Article
Language:English
Published: 2000.
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Online Access:Get fulltext

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