Neutron diffraction study of the crystallographic preferential orientation of metagabro mylonite

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21340%2F13%3A00211933" target="_blank" >RIV/68407700:21340/13:00211933 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985530:_____/13:00425485

Výsledek na webu

<a href="http://journals.cambridge.org/action/displayAbstract?fromPage=online&aid=9066591" target="_blank" >http://journals.cambridge.org/action/displayAbstract?fromPage=online&aid=9066591</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1017/S0885715613000985" target="_blank" >10.1017/S0885715613000985</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Neutron diffraction study of the crystallographic preferential orientation of metagabro mylonite

Popis výsledku v původním jazyce

Neutron diffraction (ND) was used to investigate the crystallographic preferential orientation (CPO, texture) and structure parameters of four samples of metagabro mylonite collected from the eastern part of the metagabbro sheet at the Stare Mesto belt,Bohemia Massif, Czech Republic. The samples were selected to form a deformation-ordered series with the microstructure varying from non-deformed metagabbro protolith to strongly sheared ultramylonite and amphibole-rich ulramylonite. The specimens used inND measurements were polished in form of an exact sphere with diameter 50+/-0.1 mm. The obtained ND patterns were corrected for non-linear background and then evaluated using the Rietveld method implemented in the software package GSAS. Data recorded from powder preparded by milling material from the sampled rocks were used to refine the structure parameters of plagioclase (labradorite structure, triclinic space group C-1) and amphibole (monoclinic space group C2/m). The experiments wer

Název v anglickém jazyce

Neutron diffraction study of the crystallographic preferential orientation of metagabro mylonite

Popis výsledku anglicky

Neutron diffraction (ND) was used to investigate the crystallographic preferential orientation (CPO, texture) and structure parameters of four samples of metagabro mylonite collected from the eastern part of the metagabbro sheet at the Stare Mesto belt,Bohemia Massif, Czech Republic. The samples were selected to form a deformation-ordered series with the microstructure varying from non-deformed metagabbro protolith to strongly sheared ultramylonite and amphibole-rich ulramylonite. The specimens used inND measurements were polished in form of an exact sphere with diameter 50+/-0.1 mm. The obtained ND patterns were corrected for non-linear background and then evaluated using the Rietveld method implemented in the software package GSAS. Data recorded from powder preparded by milling material from the sampled rocks were used to refine the structure parameters of plagioclase (labradorite structure, triclinic space group C-1) and amphibole (monoclinic space group C2/m). The experiments wer

Druh

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

CEP obor

BM - Fyzika pevných látek a magnetismus

OECD FORD obor

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Projekt

<a href="/cs/project/GA205%2F08%2F0767" target="_blank" >GA205/08/0767: Neutronografická texturní analýza vápenců a gaber</a><br>

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)<br>S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2013

Kód důvěrnosti údajů

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

Název periodika

Powder Diffraction

ISSN

0885-7156

e-ISSN

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Svazek periodika

28

Číslo periodika v rámci svazku

S2

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

8

Strana od-do

276-283

Kód UT WoS článku

000327314000024

EID výsledku v databázi Scopus

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