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Seismic crustal imaging using fin whale songs

Publikováno v: Science. 371:731-735

Structure from a whale song Probing the structure of the ocean crust requires a wave source. The most common source is an air gun, which is effective but potentially harmful for ocean life and not easy to use everywhere. Kuna and Nábělek found that

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bf87f4f8ff88c5168f1b3c72499a5abe
https://doi.org/10.1126/science.abf3962

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A Rapid Response Network to Record Aftershocks of the 2015 M 7.8 Gorkha Earthquake in Nepal

Autor: Abhijit Ghosh, L. B. Adhikari, John L. Nábělek, Soma Nath Sapkota, Manuel M. Mendoza, Simon L. Klemperer, Jochen Braunmiller, Marianne Karplus, M. Pant, Aaron A. Velasco, V. M. Kuna

Publikováno v: Seismological Research Letters. 91:2399-2408

The Himalaya has experienced large damaging earthquakes over the past few centuries, most recently the damaging 25 April 2015 M 7.8 Gorkha earthquake in Nepal. Because of the continued earthquake risk presented by the continental collisional plate bo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::19bd4ca8e9bed5a14259245141b02585
https://doi.org/10.1785/0220190394

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Mode of slip and crust–mantle interaction at oceanic transform faults

Autor: V. M. Kuna, Jochen Braunmiller, John L. Nábělek

Publikováno v: Nature Geoscience. 12:138-142

Oceanic transform faults, connecting offset mid-ocean spreading centres, rupture quasi-periodically in earthquakes up to about magnitude M 7.0 that are often preceded by foreshocks. In addition to seismic slip, a large portion of slip takes place as

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::233b385d928520f88cf8caca7ec21ff2
https://doi.org/10.1038/s41561-018-0287-1

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Earthquake occurrence reveals magma ascent beneath volcanoes and seamounts in the Banda region

Autor: Aleš Špičák, Jiří Vaněk, V. M. Kuna

Publikováno v: Bulletin of Volcanology. 75

Characteristic seismicity patterns beneath the volcanic arcs of the Banda region, SE Asia, suggest that magmatic processes have recently occurred beneath submarine portions of the arcs, forming yet-unrecognised submarine volcanoes. We have found that

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::09aab9e44ee5513cd01c6476b8b848b9
https://doi.org/10.1007/s00445-013-0777-3

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