Magnetic anisotropy and tectonic of the Upper Proterozoic rocks of Barrandian

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F14%3A00075451" target="_blank" >RIV/00216224:14310/14:00075451 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Magnetic anisotropy and tectonic of the Upper Proterozoic rocks of Barrandian

Popis výsledku v původním jazyce

This work represents the first results of AMS research in Kralupy-Zbraslav and Štěchovice formations. These formations are located in Barrandian from central Bohemia region among Prague, Rožmitál pod Třemšínem and Nový Knín. It is a 15?20 km wide and about 60 km long stripe of slates, siltstones, graywackes, and conglomerates. The belt is oriented in SW-NE direction and main bedding surfaces as well as cleavage planes strike approximately in the same way. Oriented samples were taken by manual drilling machine from outcrops or in laboratory from oriented stones. Cores, 25 mm in diameter and 20-25 mm length, were measured in AGICO laboratories, on MFK1 device. The first sets of samples were studied in five localities, where anisotropy of magnetic susceptibility (AMS) was measured. Orientation of principal directions of AMS is shown in azimuthal plots (see Fig. 1).

Název v anglickém jazyce

Magnetic anisotropy and tectonic of the Upper Proterozoic rocks of Barrandian

Popis výsledku anglicky

This work represents the first results of AMS research in Kralupy-Zbraslav and Štěchovice formations. These formations are located in Barrandian from central Bohemia region among Prague, Rožmitál pod Třemšínem and Nový Knín. It is a 15?20 km wide and about 60 km long stripe of slates, siltstones, graywackes, and conglomerates. The belt is oriented in SW-NE direction and main bedding surfaces as well as cleavage planes strike approximately in the same way. Oriented samples were taken by manual drilling machine from outcrops or in laboratory from oriented stones. Cores, 25 mm in diameter and 20-25 mm length, were measured in AGICO laboratories, on MFK1 device. The first sets of samples were studied in five localities, where anisotropy of magnetic susceptibility (AMS) was measured. Orientation of principal directions of AMS is shown in azimuthal plots (see Fig. 1).

Druh

O - Ostatní výsledky

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2014

Kód důvěrnosti údajů

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