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...
Main Authors: | , , , , |
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Format: | Article |
Language: | English |
Published: |
2000.
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Subjects: | |
Online Access: | Get fulltext |