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Stoletnica odkritja Mohorovičićeve diskontinuitete (meja med Zemljino skorjo in plaščem) = Centenary of the discovery of the Mohorovičić discontinuity (the boundary between the Earth's crust and its mantle)Gosar, Andrej, 1963-Hrvaški seizmolog Andrija Mohorovičić je na podlagi analiz seizmogramov potresa, ki se je zgodil pred sto leti (9. oktobra 1909) v dolini Kolpe, prvi na svetu ugotovil pomembno hitrostno ... diskontinuiteto, ki ločuje Zemljino skorjo od njenega plašča in je pozneje dobila ime Mohorovičićeva diskontinuiteta. Ugotovil je, da so na seizmogramih potresnih opazovalnic, oddaljenih med 300 in 720 km od nadžarišča potresa, vidni dvojni prihodi P in S valov. Prvi na seizmogramih sta fazi Pn in Sn, ki ustrezata daljši, lomljeni, vendar hitrejši poti skozi vrhnji del plašča. Fazi Pg in Sg ustrezata neposrednemu valovanju, ki se razširja le v Zemljini skorji, za katero so značilne manjše hitrosti potresnega valovanja. Novejše raziskave so pokazale velike razlike v globini Mohorovičićeve diskontinuitete pod Slovenijo z nekaterimi presenetljivo skokovitimi prehodi.Source: Ujma : revija za vprašanja varstva pred naravnimi in drugimi nesrečami. - ISSN 0353-085X (Št. 23, 2009, str. 314-321)Type of material - article, component partPublish date - 2009Language - slovenianCOBISS.SI-ID - 1698133
Author
Gosar, Andrej, 1963-
Topics
potresi |
seizmika |
Mohorovičićeva diskontinuiteta |
Zemljina skorja
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source: Ujma : revija za vprašanja varstva pred naravnimi in drugimi nesrečami. - ISSN 0353-085X (Št. 23, 2009, str. 314-321)
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Gosar, Andrej, 1963- | 11443 |
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