Do Active Transverse Faults Exist on the Southern Coast of Corinth Rift?
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F14%3A00440249" target="_blank" >RIV/67985530:_____/14:00440249 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Do Active Transverse Faults Exist on the Southern Coast of Corinth Rift?
Original language description
One of the most seismoactive regions of the Corinth Rift in Greece is the area around Aigion on the southwestern coast of the Gulf of Corinth. The system of active normal faults was determined by both geological and seismological studies. However, many questions persist on total slip rates on the faults, as well as the thickness and geometry of sedimentary cover of the basement formed by Mesozoic carbonates. Moreover, not enough information was available on the structural and tectonic setting between the Helike and Aigion faults. No discussions were held on possible existence and activity of transverse faults of N-S to NNE-SSW direction.
Czech name
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Czech description
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Classification
Type
D - Article in proceedings
CEP classification
DC - Seismology, volcanology and Earth structure
OECD FORD branch
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Result continuities
Project
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Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2014
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Article name in the collection
Proceedings of the 20th European Meeting of Environmental and Engineering Geophysics - Near Surface Geoscience
ISBN
978-94-6282-027-2
ISSN
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e-ISSN
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Number of pages
5
Pages from-to
"Tu PA2 06/1"-"Tu PA2 06/5"
Publisher name
EAGE
Place of publication
Houten
Event location
Athens
Event date
Sep 14, 2014
Type of event by nationality
EUR - Evropská akce
UT code for WoS article
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