Eigenvector of gravity gradient tensor for estimating fault dips considering fault type

Eigenvector of gravity gradient tensor for estimating fault dips considering fault type

Abstract The dips of boundaries in faults and caldera walls play an important role in understanding their formation mechanisms. The fault dip is a particularly important parameter in numerical simulations for hazard map creation as the fault dip affects estimations of the area of disaster occurrence...

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Bibliographic Details
Main Author: Shigekazu Kusumoto
Format: Article
Language:English
Published: SpringerOpen 2017-06-01
Series:Progress in Earth and Planetary Science
Subjects:
Fault dip
Gravity gradient tensor
Eigenvector
Normal fault
Reverse fault
Kurehayama Fault
Online Access:http://link.springer.com/article/10.1186/s40645-017-0130-0

Internet

http://link.springer.com/article/10.1186/s40645-017-0130-0

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