| NEHYBA, Slavomír a Daniel NÝVLT. Deposits of pyroclastic mass flows at Bibby Hill (Pliocene, James Ross Island, Antarctica). CZECH POLAR REPORTS. Brno: Masarykova Univerzita, roč. 4, č. 2, s. 103-122. ISSN 1805-0689. doi:10.5817/CPR2014-2-11. 2014. |
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@article{1220365,
author = {Nehyba, Slavomír and Nývlt, Daniel},
article_location = {Brno},
article_number = {2},
doi = {http://dx.doi.org/10.5817/CPR2014-2-11},
keywords = {pyroclastic currents-pyroclastic flows-resedimented pyroclastic deposits},
language = {eng},
issn = {1805-0689},
journal = {CZECH POLAR REPORTS},
title = {Deposits of pyroclastic mass flows at Bibby Hill (Pliocene, James Ross Island, Antarctica)},
volume = {4},
year = {2014}
}
TY - JOUR
ID - 1220365
AU - Nehyba, Slavomír - Nývlt, Daniel
PY - 2014
TI - Deposits of pyroclastic mass flows at Bibby Hill (Pliocene, James Ross Island, Antarctica)
JF - CZECH POLAR REPORTS
VL - 4
IS - 2
SP - 103-122
EP - 103-122
PB - Masarykova Univerzita
SN - 18050689
KW - pyroclastic currents-pyroclastic flows-resedimented pyroclastic deposits
N2 - Sedimentological study of the southern slopes of Bibby Hill (relic of a Pliocene tuff cone) allows recognition of twelve lithofacies and three facies associations. Deposits of pyroclastic currents (both low- and high density pyroclastic currents) dominate over the deposits of pyroclastic flows. Products of suabaerial resedimented pyroclastic deposits play minor role. Vertical distribution of facies associations within the studied succession is not uniform. These differences in the distribution of facies associations are interpreted as response to variations in the intensity and type (Surtseyan, Taalian) of phreatomagmatic eruptions, water availability and morphology of the cone.
ER -
NEHYBA, Slavomír a Daniel NÝVLT. Deposits of pyroclastic mass flows at Bibby Hill (Pliocene, James Ross Island, Antarctica). \textit{CZECH POLAR REPORTS}. Brno: Masarykova Univerzita, roč.~4, č.~2, s.~103-122. ISSN~1805-0689. doi:10.5817/CPR2014-2-11. 2014.
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