KOTKOVÁ, Jana, Simon HARLEY and Milan FIŠERA. A vestige of very high - pressure (ca. 28 kbar) metamorphism in the Variscan Bohemian Massif, Czech Republic. European Journal of Mineralogy. Německo, 1997, vol. 9, p. 1017-1032. ISSN 0935-1221.
Other formats:   BibTeX LaTeX RIS
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
Original language English
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher Germany
Confidentiality degree is not subject to a state or trade secret
Impact factor Impact factor: 1.099
Organization unit Faculty of Science
Keywords in English garnetite; orthopyroxene; very-high pressure; Bohemian Massif
Tags Bohemian massif, garnetite, orthopyroxene, very-high pressure
Changed by Changed by: doc. RNDr. Jana Kotková, CSc., učo 54844. Changed: 7/12/2001 12:45.
Abstract
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.
PrintDisplayed: 13/5/2024 08:40