About: Determination of field-independent and field-dependent components of anisotropy of susceptibility through standard AMS measurement in variable low fields II:

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About: Determination of field-independent and field-dependent components of anisotropy of susceptibility through standard AMS measurement in variable low fields II: Goto Sponge NotDistinct Permalink

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rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
Description	A large ultramafic body (garnet clinopyroxenite and garnet peridotite) embedded in felsic granulite at Bory (Moldanubian Zone of Western Moravia, Czech Republic) contains multiple carrier of susceptibility. Low-field variation of anisotropy of magnetic susceptibility (AMS) enables the separation of the field independent and low-field dependent AMS components to be made. A large ultramafic body (garnet clinopyroxenite and garnet peridotite) embedded in felsic granulite at Bory (Moldanubian Zone of Western Moravia, Czech Republic) contains multiple carrier of susceptibility. Low-field variation of anisotropy of magnetic susceptibility (AMS) enables the separation of the field independent and low-field dependent AMS components to be made. (en)
Title	Determination of field-independent and field-dependent components of anisotropy of susceptibility through standard AMS measurement in variable low fields II: Determination of field-independent and field-dependent components of anisotropy of susceptibility through standard AMS measurement in variable low fields II: (en)
skos:prefLabel	Determination of field-independent and field-dependent components of anisotropy of susceptibility through standard AMS measurement in variable low fields II: Determination of field-independent and field-dependent components of anisotropy of susceptibility through standard AMS measurement in variable low fields II: (en)
skos:notation	RIV/00216208:11310/09:10000142!RIV10-GA0-11310___
http://linked.open...avai/riv/aktivita	P Z
http://linked.open...avai/riv/aktivity	P(GA205/06/0688), Z(AV0Z30120515), Z(MSM0021620855)
http://linked.open...iv/cisloPeriodika	1-2
http://linked.open...vai/riv/dodaniDat	2010
http://linked.open...aciTvurceVysledku	Faryad, Shah Wali Hrouda, František Kratinová, Zuzana Jeřábek, Petr
http://linked.open.../riv/druhVysledku	J - Článek v odborném periodiku
http://linked.open...iv/duvernostUdaju	S - Úplné a pravdivé údaje nepodléhající ochraně podle zvláštních právních předpisů
http://linked.open...titaPredkladatele	Univerzita Karlova v Praze / Přírodovědecká fakulta
http://linked.open...dnocenehoVysledku	309899
http://linked.open...ai/riv/idVysledku	RIV/00216208:11310/09:10000142
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	Determination; field-independent; and; field-dependent; components; anisotropy; susceptibility; through; standard; AMS; measurement; variable; low; fields; II: (en)
http://linked.open.../riv/klicoveSlovo	variable field-dependent field-independent anisotropy components measurement susceptibility Determination fields AMS and standard low through II:
http://linked.open...odStatuVydavatele	NL - Nizozemsko
http://linked.open...ontrolniKodProRIV	[F929B5E89888]
http://linked.open...i/riv/nazevZdroje	Tectonophysics
http://linked.open...in/vavai/riv/obor	DB
http://linked.open...ichTvurcuVysledku	4 (xsd:int)
http://linked.open...cetTvurcuVysledku	5 (xsd:int)
http://linked.open...vavai/riv/projekt	Thermal history and petrological model(s) for formation and exhumation of HP andUHP rocks during Variscan orogeny in the Bohemian Massif
http://linked.open...UplatneniVysledku	2009
http://linked.open...v/svazekPeriodika	466
http://linked.open...iv/tvurceVysledku	Hrouda, František Jeřábek, Petr Faryad, Shah Wali Chlupáčová, Marta Kratinová, Zuzana
http://linked.open...ain/vavai/riv/wos	000264470600011
http://linked.open...n/vavai/riv/zamer	Study of the internal structure and dynamics of the Earth Material flow mechanisms in the upper spheres of the Earth
issn	0040-1951
number of pages	12 (xsd:int)
http://localhost/t...ganizacniJednotka	11310

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