Detailed Information on Publication Record

NEHYBA, Slavomír. Coarse grain deltas along the margins of the peripheral foreland basin (Neogene, Carpathian Foredeep). In B. Bádenas, M. Aurell and A.M. Alonso-Zarza. Abstracts, 28th IAS Meeting of Sedimentology, Zaragoza, Spain. Zaragoza: International Association of Sedimentologists, 2011, p. 444-444. ISBN 978-84-615-1755-8.

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Basic information
Original name	Coarse grain deltas along the margins of the peripheral foreland basin (Neogene, Carpathian Foredeep)
Name in Czech	Hrubozrnné delty podél okrajů okrajové předpolní pánve (neogén, karpatská předhlubeň)
Authors	NEHYBA, Slavomír.
Edition	Zaragoza, Abstracts, 28th IAS Meeting of Sedimentology, Zaragoza, Spain, p. 444-444, 1 pp. 2011.
Publisher	International Association of Sedimentologists

Other information
Original language	English
Type of outcome	Proceedings paper
Field of Study	10500 1.5. Earth and related environmental sciences
Country of publisher	Spain
Confidentiality degree	is not subject to a state or trade secret
Organization unit	Faculty of Science
ISBN	978-84-615-1755-8
Keywords (in Czech)	hrubozrnné delty, okrajová předpolní pánev
Keywords in English	coarse grain deltas, peripheral foreland basin
Tags	International impact, Reviewed
Changed by	Changed by: prof. RNDr. Slavomír Nehyba, Dr., učo 2710. Changed: 19/8/2011 07:41.

Abstract
Coarse grain deltas located along both “active” and “passive” margins of the foreland basins differ in provenance. Provenance study is based on the pebble analyses, heavy minerals associations, and garnet and rutile geochemistry. Gravels are polymict and the composition of each delta body is strongly influenced by the local sources (Precambrian crystalline rocks, Palaeozoic graywackes and shales, Mesozoic carbonates). Abundant presence of intraclasts (sometimes several m in diameter) reflects cannibalisation of the older basin infill.

Abstract

Coarse grain deltas located along both “active” and “passive” margins of the foreland basins differ in provenance. Provenance study is based on the pebble analyses, heavy minerals associations, and garnet and rutile geochemistry. Gravels are polymict and the composition of each delta body is strongly influenced by the local sources (Precambrian crystalline rocks, Palaeozoic graywackes and shales, Mesozoic carbonates). Abundant presence of intraclasts (sometimes several m in diameter) reflects cannibalisation of the older basin infill.

Abstract (in Czech)
Coarse grain deltas located along both “active” and “passive” margins of the foreland basins differ in provenance. Provenance study is based on the pebble analyses, heavy minerals associations, and garnet and rutile geochemistry. Gravels are polymict and the composition of each delta body is strongly influenced by the local sources (Precambrian crystalline rocks, Palaeozoic graywackes and shales, Mesozoic carbonates). Abundant presence of intraclasts (sometimes several m in diameter) reflects cannibalisation of the older basin infill.

Abstract (in Czech)

Links
GA205/09/0103, research and development project	Name: Mělkovodní ekosystémy středního miocénu Centrální Paratethydy: Sukcese a interakce anorganické a organické složky ekosystémů
GA205/09/0103, research and development project	Investor: Czech Science Foundation