J 1997

A vestige of very high - pressure (ca. 28 kbar) metamorphism in the Variscan Bohemian Massif, Czech Republic

KOTKOVÁ, Jana, Simon HARLEY and Milan FIŠERA

Basic information

Original name

A vestige of very high - pressure (ca. 28 kbar) metamorphism in the Variscan Bohemian Massif, Czech Republic

Authors

KOTKOVÁ, Jana, Simon HARLEY and Milan FIŠERA

Edition

European Journal of Mineralogy, Německo, 1997, 0935-1221

Other information

Language

English

Type of outcome

Článek v odborném periodiku

Field of Study

10500 1.5. Earth and related environmental sciences

Country of publisher

Germany

Confidentiality degree

není předmětem státního či obchodního tajemství

Impact factor

Impact factor: 1.099

Organization unit

Faculty of Science

Keywords in English

garnetite; orthopyroxene; very-high pressure; Bohemian Massif

Tags

Změněno: 7/12/2001 12:45, doc. RNDr. Jana Kotková, CSc.

Abstract

V originále

Pyropic garnetite from the Podolsko Complex, south Bohemian Moldanubian Zone, Bohemian Massif, records very-high pressure (28kbar, 830 deg.C)conditions of formation of the initial mineral assemblage. As such it represents the first evidence for very-high pressure metamorphism of continental crustal material in the Moldanubian Zone of the Bohemian Massif. This assemblage was extensively overprinted by complex symplectites, formed during a subsequent medium-pressure high-temperature event.