Provenance of the Lower Carboniferous Culm sediments of the Drahany Upland (Czech Republic), derived from garnet chemistry

ČOPJAKOVÁ, Renata, Petr SULOVSKÝ and Jiří OTAVA. Provenance of the Lower Carboniferous Culm sediments of the Drahany Upland (Czech Republic), derived from garnet chemistry. Mitteilungen der Österr. Mineral. Gesellschaft. Wien: Bundesministerium für Wissenschaft, Wien, 2001, vol. 146, September, p. 58-60. ISSN 1609-0144.

Basic information

Original name

Provenance of the Lower Carboniferous Culm sediments of the Drahany Upland (Czech Republic), derived from garnet chemistry

Authors

ČOPJAKOVÁ, Renata (203 Czech Republic), Petr SULOVSKÝ (203 Czech Republic) and Jiří OTAVA

Edition

Mitteilungen der Österr. Mineral. Gesellschaft, Wien, Bundesministerium für Wissenschaft, Wien, 2001, 1609-0144

---

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

Austria

Confidentiality degree

není předmětem státního či obchodního tajemství

RIV identification code

RIV/00216224:14310/01:00004957

Organization unit

Faculty of Science

Keywords in English

garnet chemistry; sediment provenance; Culm; Drahany Upland

Tags

Culm, Drahany Upland, garnet chemistry, sediment provenance

---

Abstract

V originále

The provenance of Culm sediments was deciphered using the specific features of detrital garnet chemistry. The study revealed a sudden change in source area within the Myslejovice Formation.

---

Links

GA205/99/0567, research and development project

Name: Odraz exhumace variské spodní kůry ve složení viséských siliciklastik (východní okraj Českého masivu) Investor: Czech Science Foundation, Exhumation of the Variscan lower crust - constraints Viséan siliciclastics (Eastern Bohemian Massif)