Depositional settings of the Pleistocene continental glaciation
sediments in the foothills of Rychleby Mountains and Zlate Hory
Highlands, Sudetes Mts., Czechia

D 2013

Depositional settings of the Pleistocene continental glaciation sediments in the foothills of Rychleby Mountains and Zlate Hory Highlands, Sudetes Mts., Czechia

HANÁČEK, Martin, Daniel NÝVLT a Slavomír NEHYBA

Základní údaje

Originální název

Depositional settings of the Pleistocene continental glaciation sediments in the foothills of Rychleby Mountains and Zlate Hory Highlands, Sudetes Mts., Czechia

Autoři

HANÁČEK, Martin, Daniel NÝVLT a Slavomír NEHYBA

Vydání

Warszawa, XX Konferencja Stratygrafia plejstocenu Polski Plejstocen przedpola Sudetów Środkowych Lasocin, 2.-6. 09. 2013 r. od s. 51-55, 5 s. 2013

Nakladatel

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Další údaje

Jazyk

angličtina

Typ výsledku

Stať ve sborníku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Česká republika

Utajení

není předmětem státního či obchodního tajemství

Forma vydání

tištěná verze "print"

Organizační jednotka

Přírodovědecká fakulta

ISBN

978-83-7863-259-7

Klíčová slova anglicky

glacitectonite ablation moraines terminoglacial fan proglacial outwash plain glaciofluvial sediments glaciolacustrine sediments diamictite continental glaciation pleistocene Rychleby Mts. Zlaté Hory Highlands Sudetes Mts. Czechia

Změněno: 10. 9. 2013 13:01, Mgr. Martin Hanáček, Ph.D.

Anotace

V originále

Northern European ice sheet advanced during its maximum Elsterian extent to the Central and Eastern Sudetes Mts. foreland, i.e. to the Rychleby Mts. and Zlaté Hory Highlands. Glacial deposition was controlled by local morphology in this area. The following depositional environments have been identified during ongoing research in Rychleby Mts. and Zlaté Hory Highlands: subglacial environment affected by subglacial morphology and lithology (cavities infill, glacitectonite), supraglacial environment of ablation moraines, terminoglacial to proglacial outwash plains, terminoglacial fans and proglacial outwash plains.

Citovat

HANÁČEK, Martin, Daniel NÝVLT a Slavomír NEHYBA. Depositional settings of the Pleistocene continental glaciation sediments in the foothills of Rychleby Mountains and Zlate Hory Highlands, Sudetes Mts., Czechia. In XX Konferencja Stratygrafia plejstocenu Polski Plejstocen przedpola Sudetów Środkowych Lasocin, 2.-6. 09. 2013 r. Warszawa: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy, 2013, s. 51-55. ISBN 978-83-7863-259-7.

@inproceedings{1121827,
   author = {Hanáček, Martin and Nývlt, Daniel and Nehyba, Slavomír},
   address = {Warszawa},
   booktitle = {XX Konferencja Stratygrafia plejstocenu Polski Plejstocen przedpola Sudetów Środkowych Lasocin, 2.-6. 09. 2013 r.},
   keywords = {glacitectonite ablation moraines terminoglacial fan proglacial outwash plain glaciofluvial sediments glaciolacustrine sediments diamictite continental glaciation pleistocene Rychleby Mts. Zlaté Hory Highlands Sudetes Mts. Czechia},
   howpublished = {tištěná verze "print"},
   language = {eng},
   location = {Warszawa},
   isbn = {978-83-7863-259-7},
   pages = {51-55},
   publisher = {Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy},
   title = {Depositional settings of the Pleistocene continental glaciation sediments in the foothills of Rychleby Mountains and Zlate Hory Highlands, Sudetes Mts., Czechia},
   year = {2013}
}

TY  - JOUR
ID  - 1121827
AU  - Hanáček, Martin - Nývlt, Daniel - Nehyba, Slavomír
PY  - 2013
TI  - Depositional settings of the Pleistocene continental glaciation sediments in the foothills of Rychleby Mountains and Zlate Hory Highlands, Sudetes Mts., Czechia
PB  - Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
CY  - Warszawa
SN  - 9788378632597
KW  - glacitectonite ablation moraines terminoglacial fan proglacial outwash plain glaciofluvial sediments glaciolacustrine sediments diamictite continental glaciation pleistocene Rychleby Mts. Zlaté Hory Highlands Sudetes Mts. Czechia
N2  - Northern European ice sheet advanced during its maximum Elsterian extent to the Central and Eastern Sudetes Mts. foreland, i.e. to the Rychleby Mts. and Zlaté Hory Highlands. Glacial deposition was controlled by local morphology in this area. The following depositional environments have been identified during ongoing research in Rychleby Mts. and Zlaté Hory Highlands: subglacial environment affected by subglacial morphology and lithology (cavities infill, glacitectonite), supraglacial environment of ablation moraines, terminoglacial to proglacial outwash plains, terminoglacial fans and proglacial outwash plains.
ER  -

HANÁČEK, Martin, Daniel NÝVLT a Slavomír NEHYBA. Depositional settings of the Pleistocene continental glaciation sediments in the foothills of Rychleby Mountains and Zlate Hory Highlands, Sudetes Mts., Czechia. In \textit{XX Konferencja Stratygrafia plejstocenu Polski Plejstocen przedpola Sudetów \'Srodkowych Lasocin, 2.-6. 09. 2013 r.}. Warszawa: Pa\'nstwowy Instytut Geologiczny - Pa\'nstwowy Instytut Badawczy, 2013, s.~51-55. ISBN~978-83-7863-259-7.

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