Magnetic fabric of the Říčany granite, Bohemian Massif

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F10%3A00000282" target="_blank" >RIV/00025798:_____/10:00000282 - isvavai.cz</a>

Result on the web

—

DOI - Digital Object Identifier

—

Result language

angličtina

Original language name

Magnetic fabric of the Říčany granite, Bohemian Massif

Original language description

The Říčany pluton represents an elliptical shallow-level intrusion made up of outer, more fractionated, strongly porphyritic granite and inner, less evolved, weakly porphyritic granite. Mesoscopic foliation defines an onion-skin pattern and corresponds well to the magnetic (AMS) foliations. Magnetic lineation plunges shallowly (0-20°) and is subparallel to the contact in the outer part of the pluton, whereas in the pluton center lineation dips steeply (60-70°) with variable trends. We interpret the fabrics in the pluton as being a result of helical flow, whereby faster subvertical flow in the low-viscosity pluton center generated subhorizontal flow in the outer, higher-viscosity (phenocrystrich)margin.

Czech name

—

Czech description

—

Type

J_x - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

CEP classification

DB - Geology and mineralogy

OECD FORD branch

—

Project

—

Continuities

Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year

2010

Confidentiality

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

Name of the periodical

Trabajos de Geología

ISSN

0474-9588

e-ISSN

—

Volume of the periodical

30

Issue of the periodical within the volume

1

Country of publishing house

ES - SPAIN

Number of pages

7

Pages from-to

—

UT code for WoS article

—

EID of the result in the Scopus database

—