- Abstract:
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The presence of fault scarps is a first-order criterion for identifying active faults. Yet the preservation of these features depends on the recurrence interval between surface rupturing events, combined with the rates of erosional and depositional processes that act on the landscape. Within arid continental interiors single earthquake scarps can be preserved for thousands of years, and yet the interval between surface ruptures on faults in these regions may be much longer, such that the lack...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Publisher's version
- Files:
-
-
(pdf, 6.1mb)
-
- Publisher copy:
- 10.1016/j.epsl.2016.11.025
-
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- Publisher:
- Elsevier Publisher's website
- Journal:
- Earth and Planetary Science Letters Journal website
- Volume:
- 459
- Pages:
- 93-104
- Publication date:
- 2016-11-30
- Acceptance date:
- 2016-11-15
- DOI:
- EISSN:
-
1385-013X
- ISSN:
-
0012-821X
- Pubs id:
-
pubs:659738
- URN:
-
uri:3b4350ea-dbee-429c-9a42-55de799aa179
- UUID:
-
uuid:3b4350ea-dbee-429c-9a42-55de799aa179
- Local pid:
- pubs:659738
- Copyright holder:
- C. Grützner et al.
- Copyright date:
- 2016
- Notes:
- © 2016 The Authors. Published by Elsevier B.V. Open Access funded by Natural Environment Research Council, available under a Creative Commons license.
Journal article
Assessing the activity of faults in continental interiors: palaeoseismic insights from SE Kazakhstan
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Centre for Observation and Modelling of Earthquakes and Tectonics
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