Kyanite Pseudomorphs after Andalusite from the Teplá Crystalline Complex - Evidence for Pre-Variscan Low-Pressure Metamorphism

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F99%3A00000281" target="_blank" >RIV/00025798:_____/99:00000281 - isvavai.cz</a>

Result on the web

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DOI - Digital Object Identifier

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Result language

angličtina

Original language name

Kyanite Pseudomorphs after Andalusite from the Teplá Crystalline Complex - Evidence for Pre-Variscan Low-Pressure Metamorphism

Original language description

A narrow horizon of quartz-kyanite segregations, about 11 km long occurs in the south of the Teplá Crystalline Complex. Kyanite represents pseudomorphs after older andalusite originated during the M2 HP event (570-640 °C, 6.5-9.5 Kb)

Czech name

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Czech description

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Type

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

CEP classification

DB - Geology and mineralogy

OECD FORD branch

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Project

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Continuities

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Publication year

1999

Confidentiality

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

Name of the periodical

Geolines

ISSN

1210-9606

e-ISSN

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Volume of the periodical

8

Issue of the periodical within the volume

x

Country of publishing house

CZ - CZECH REPUBLIC

Number of pages

2

Pages from-to

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UT code for WoS article

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EID of the result in the Scopus database

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