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Part VI - Modelling of Glacially Induced Faults and Stress

Published online by Cambridge University Press:  02 December 2021

Holger Steffen
Affiliation:
Lantmäteriet, Sweden
Odleiv Olesen
Affiliation:
Geological Survey of Norway
Raimo Sutinen
Affiliation:
Geological Survey of Finland
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Summary

As glacially induced faults are reactivated due to a combination of tectonic and glacially induced isostatic stresses, it is interesting to model the corresponding fault slip with dedicated models. The next chapters introduce first such a modelling approach with a well-established model of glacial isostatic adjustment followed by a review of stresses to be considered in sophisticated future modelling.

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Publisher: Cambridge University Press
Print publication year: 2021

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References

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Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

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Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

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Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

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