Complex local Moho topography in the Western Carpathians: Indication of the ALCAPA and the European Plate contact

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F15%3A00433253" target="_blank" >RIV/67985530:_____/15:00433253 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.tecto.2014.10.013" target="_blank" >http://dx.doi.org/10.1016/j.tecto.2014.10.013</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.tecto.2014.10.013" target="_blank" >10.1016/j.tecto.2014.10.013</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Complex local Moho topography in the Western Carpathians: Indication of the ALCAPA and the European Plate contact

Popis výsledku v původním jazyce

Seismic data from deep refraction and wide-angle reflection profiles intersecting the Western Carpathians show distinct upper-mantle Pn phases with anomalous apparent velocities identified in the first and later arrivals. Their systematic analysis indicates that such phases are present in numerous seismic sections both for in-line and off-line shots. They are observed in data from profiles intersecting the Carpathians in the west at the contact with the Bohemian Massif; similar feature was also found indata at the northern edge of the Carpathians at the contact with the North European Platform. Modelling of these anomalous Pn phases shows that they originate due to local structural anomalies of the Moho discontinuity detected in several places along the Western Carpathian arc. Such anomalies are located in close lateral proximity of the Pieniny Klippen Belt representing the contact between the stable European Plate in the north and the ALCAPA (Alpine-Carpathian-Pannonian) microplate i

Název v anglickém jazyce

Complex local Moho topography in the Western Carpathians: Indication of the ALCAPA and the European Plate contact

Popis výsledku anglicky

Seismic data from deep refraction and wide-angle reflection profiles intersecting the Western Carpathians show distinct upper-mantle Pn phases with anomalous apparent velocities identified in the first and later arrivals. Their systematic analysis indicates that such phases are present in numerous seismic sections both for in-line and off-line shots. They are observed in data from profiles intersecting the Carpathians in the west at the contact with the Bohemian Massif; similar feature was also found indata at the northern edge of the Carpathians at the contact with the North European Platform. Modelling of these anomalous Pn phases shows that they originate due to local structural anomalies of the Moho discontinuity detected in several places along the Western Carpathian arc. Such anomalies are located in close lateral proximity of the Pieniny Klippen Belt representing the contact between the stable European Plate in the north and the ALCAPA (Alpine-Carpathian-Pannonian) microplate i

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DC - Seismologie, vulkanologie a struktura Země

OECD FORD obor

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Projekt

<a href="/cs/project/GA13-08971S" target="_blank" >GA13-08971S: STAVBA KŮRY URČENÁ Z ANALÝZY VLNOVÝCH OBRAZŮ LOKÁLNÍCH MIKROZEMĚTŘESENÍ</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Tectonophysics

ISSN

0040-1951

e-ISSN

—

Svazek periodika

638

Číslo periodika v rámci svazku

7 January

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

19

Strana od-do

63-81

Kód UT WoS článku

000348266400003

EID výsledku v databázi Scopus

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