Bounding relationships between parameters of earthquakes and seismogenic clastic dikes (based on worldwide data)
- Authors: Lunina O.V.1, Gladkov A.S.1
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Affiliations:
- Institute of the Earth’s Crust, Siberian Branch
- Issue: Vol 476, No 1 (2017)
- Pages: 978-981
- Section: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/190656
- DOI: https://doi.org/10.1134/S1028334X17090057
- ID: 190656
Cite item
Abstract
This paper presents the first boundary equations describing the relationship between earthquake parameters (magnitude MS and macroseismic intensity IP at the observation point on the MSK-64 scale) and clastic dikes (having maximal thickness mcd, visible height hcd, and the index of manifestation intensity of dikes in the cross section Icd). As was expected, the maximal size of dikes grows with an increase in the earthquake magnitude and macroseismic intensity. Analysis of the dependences showed that it is better to use all three parameters for estimation of the minimal threshold MS or IP from clastic dikes, and, in the absence of data on seismogenic rupture, the maximal calculated value should be used. Some limitations in application and the advantages of the equations obtained are discussed with respect to characterizing earthquakes of the pre-instrumental period.
About the authors
O. V. Lunina
Institute of the Earth’s Crust, Siberian Branch
Author for correspondence.
Email: lounina@crust.irk.ru
Russian Federation, Irkutsk, 664033
A. S. Gladkov
Institute of the Earth’s Crust, Siberian Branch
Email: lounina@crust.irk.ru
Russian Federation, Irkutsk, 664033
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