Seismic architecture of the tip of the Hel Peninsula, Poland

Maria Rucińska-Zjadacz , Stanisław Rudowski , Radosław Wróblewski

Abstract

The article presents results of a pioneering research on the main geological features of the Hel Peninsula based on the analysis of seismic profiles and their comparison with geological cross-sections made on the basis of drillings. The following three parts of the tip structure have been identified: barrier basement (1), barrier core (2) and barrier upper part(3). Seismic facies distinguished therein were subsequently geologically interpreted as follows: Cretaceous marl and limestone (1.1), glacial till and diamicton (1.2), silt and clay of limnoglacial/limnic/marine origin (1.3), barrier sand of the core (2), and sand and peat of the barrier upper part(3). Geological cross-sections covering the geological structure of the tip of the Hel Peninsula underwater slope and the surrounding seabed. The slope base and the distal sand colluvium extent on the seafloor were determined. This paper is the first to present a crosswise section in this part of the Hel Peninsula.
Author Maria Rucińska-Zjadacz (FOG / IO / DMG)
Maria Rucińska-Zjadacz,,
- Division of Marine Geology
, Stanisław Rudowski
Stanisław Rudowski,,
-
, Radosław Wróblewski (FOG / IG / DGQG)
Radosław Wróblewski,,
- Department of Geomorphology and Quarternary Geology
Journal seriesBaltica, ISSN 0067-3064, (A 15 pkt)
Issue year2018
Vol31
No1
Pages63-72
Publication size in sheets0.5
Keywords in Englishseismic profiling, seismic facies, sandy barrier, Gulf of Gdańsk
DOIDOI:10.5200/baltica.2018.31.06
URL http://www.gamtostyrimai.lt/uploads/documents/lediniai/Baltica/Vol-31-1-2018/Baltica%202018%20(31-1)%206%20Rucinska%20et%20al.pdf
Languageen angielski
Score (nominal)15
ScoreMinisterial score = 15.0, 09-11-2018, ArticleFromJournal
Ministerial score (2013-2016) = 15.0, 09-11-2018, ArticleFromJournal
Publication indicators WoS Impact Factor: 2016 = 0.538 (2) - 2016=0.431 (5)
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