Cordierite-bearing rocks and their relation to the PT evolution of rocks in the N parts of the Zábřeh and Polička crystaline complexes.

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F01%3A09013147" target="_blank" >RIV/67985831:_____/01:09013147 - isvavai.cz</a>

Result on the web

—

DOI - Digital Object Identifier

—

Result language

angličtina

Original language name

Cordierite-bearing rocks and their relation to the PT evolution of rocks in the N parts of the Zábřeh and Polička crystaline complexes.

Original language description

In Zábřeh Crystalline Unit the rocks with mineral assemblage Bt +St + Grt + Pl + Sill(Ky) Ms preserved conditions close to the peak metamorphic conditions, i. e. around 660 and 10 kbar. During the subsequent exhumation the pressure dropped and temperature increased to reach the conditions of a temperature maximum > 700 C at 7 kbar. The conditions of contact metamorphism were estimated at 5 to 6 kbar and 600 to 700 C. Conditions of the formation of similar rocks in the northern part of the PCC were different - 565 C and 2,5-3 kbar.

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)

Publication year

2001

Confidentiality

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

Name of the periodical

Geolines

ISSN

1210-9606

e-ISSN

—

Volume of the periodical

13

Issue of the periodical within the volume

N/A

Country of publishing house

CZ - CZECH REPUBLIC

Number of pages

1

Pages from-to

95

UT code for WoS article

—

EID of the result in the Scopus database

—