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1

Redefinition of parts of the Vimsodden Subgroup and the Deilegga Group [Proterozoic], SE Wedel Jarlsberg Land, Spitsbergen

100%
Birkenmajer K.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
1993
|
tom 41
|
nr 3
2

Lithostratigraphy of the Miocene deposits in the Gliwice Area [Upper Silesia, Poland]

100%
Alexandrowicz S. W.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
1997
|
tom 45
|
nr 2-4
3

Ice dynamics during the deglaciation of SW Skane, South Sweden

100%
Lagerlund E.
Quaestiones Geographicae. Zeszyt Specjalny
|
1995
|
tom 04
4

Correlation of Proterozoic and Cambrian lithostratigraphic units across Torellbreen, Wedel Jarlsberg Land, Spitsbergen

84%
Birkenmajer K.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
1994
|
tom 42
|
nr 4
5

Pleistocene stratigraphy of the central part of Silesian Lowland, Southwestern Poland

84%
Czerwonka J. A., Krzyszkowski D.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
1992
|
tom 40
|
nr 3
6

Type section of the Bravaisberget Formation [Middle Triassic] at Bravaisberget, Western Nathorst Land, Spitsbergen, Svalbard

84%
Krajewski K. P., Karcz P., Wozny E., Mork A.
Polish Polar Research
|
2007
|
tom 28
|
nr 2
The Bravaisberget Formation in Spitsbergen embraces an organic carbon-rich, clastic sequence that reflects a general shallow shelf development of the Middle Triassic depositional system in Svalbard. New observations and measurements of the type section of the formation at Bravaisberget in western Nathorst Land allow to present detailed litho- stratigraphical subdivision of the formation, and aid to reconstruct its depositional history. The subdivision of the formation (209 m thick at type section) into the Passhatten, Somovbreen, and Van Keulenfjorden members is sustained after Mørk et al. (1999), though with new position of the boundary between the Passhatten and Somovbreen mbs. The Passhatten Mb is defined to embrace the black shale-dominated sequence that forms the lower and middle parts of the formation (160 m thick). The Somovbreen Mb (20 m thick) is confined to the overlying, calcite-cemented sequence of marine sandstones. The Van Keulenfjorden Mb (29 m thick) forms the topmost part of the formation composed of siliceous and dolomitic sandstones. The formation is subdivided into twelve informal units, out of which eight is defined in the Passhatten Mb (units 1 to 8), two in the Somovbreen Mb (units 9 and 10), and also two in the Van Keulenfjorden Mb (units 11 and 12). Units 1, 3,5,7 and 9 contain noticeable to abundant phosphorite, and are interspaced by four black shale sequences (units 2,4,6, and 8). Unit 9 passes upwards gradually into the main sandstone sequence (unit 10) of the Somovbreen Mb. The base of the Van Keulenfjorden Mb is a discontinuity surface covered by thin phosphorite lag. The Van Keulenfjorden Mb consists of two superimposed sandstone units (units 11 and 12) that form indistinct coarsening-upward sequences. The Bravaisberget Fm records two consequent transgressive pulses that introduced high biological productivity conditions to the shelf basin. The Passhatten Mb shows pronounced repetition of sediment types resulting from interplay between organic-prone, fine-grained environments, and clastic bar environments that focused phosphogenesis. The lower part of the member (units 1 to 5) contains well-developed bar top sequences with abundant nodular phosphorite, which are under- and overlain by the bar side sequences grading into silt- to mud-shale. The upper part of the member (units 6 to 8) is dominated by mud-shale, showing the bar top to side sequence with recurrent phosphatic grainstones in its middle part. Maximum stagnation and deep-water conditions occurred during deposition of the topmost shale sequence (unit 8). Rapid shallowing trend terminated organic-rich environments of the Passhatten Mb, and was associated with enhanced phosphogenesis at base of the Somovbreen Mb (unit 9). Bioturbated sandstones of the Somovbreen Mb (unit 10) record progradation of shallow-marine clastic environments. The sequence of the Van Keulenfjorden Mb (units 11 and 12) was deposited in brackish environments reflecting closure of the Middle Triassic basin in western Svalbard.
7

Proterozoic and Palaeozoic formations in central Sorkapp Land, South Spitsbergen

84%
Birkenmajer K.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
1994
|
tom 42
|
nr 4
8

Professor Stefan Kozarski. Bibliography

84%
Quaestiones Geographicae. Zeszyt Specjalny
|
1995
|
tom 04
9

The Weddell Sea Formation: post-Late Pliocene terrestrial glacial deposits on Seymour Island, Antarctic Peninsula

67%
Gazdzicki A., Tatur A., Hara U., Del Valle R. A.
Polish Polar Research
|
2004
|
tom 25
|
nr 3-4
189-204
10
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The Frasnian-Famennian events in a deep-shelf succession, Subpolar Urals: biotic, depositional, and geochemical records

67%
Yudina A. B., Racki G., Savage N. M., Racka M., Malkowski K.
Acta Palaeontologica Polonica
|
2002
|
tom 47
|
nr 2
The Frasnian–Famennian (F–F) boundary is well biostratigraphically documented in the Palmatolepis−rich deposits exposed along the Syv’yu River in the lower slopes of the Subpolar Urals. The thin−bedded calcareous−clayey−siliceous deep−slope succession of the Vorota Formation appears to represent continuous Domanic−type deposition throughout the world−wide carbonate crisis time, without evidence for the basal Famennian hiatus or a large−scale sedimentary perturbation within a regressive setting. The northernmost Laurussian sequence exhibits many well known signatures throughout the broad F–F timespan: the appearance of organicand clay−rich deposits, icriodontid and radiolarian blooms, and a correlative shift of several geochemical proxies towards hypoxic and high−productivity regimes, perfectly recorded by positive 13Ccarb excursions of +3.5‰. Integrative biotic, microfacies and geochemical data substantiate a longer−term oceanographic destabilization, attributable to multiple Earth−bound triggering factors in (episodically enhanced?) greenhouse climate and punctuated eustatic sea−level highstands, superimposed on the elevated deposition of organic carbon−rich sediments during the Upper Kellwasser Event. Unsteady eutrophicated, and oxygen−depleted ecosystems during the F–F biotic crisis interval could be assumed, especially when intensified by various spasmodic tectono−volcanic phenomena in the incipiently closing Ural Ocean.
11

Stratigraphical position of the Obolus sandstones [Upper Cambrian-?Lowermost Ordovician] in Poland

67%
Bednarczyk W. S.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
1998
|
tom 46
|
nr 1
12

The Magnethgda sequence [Hecla Hoek Succession], NW Torell Land, Spitsbergen: a revision of lithostratigraphy and age

67%
Birkenmajer K.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
2002
|
tom 50
|
nr 2
13

The Ferdynandow Interglacial at Stanislawice near Kozienice [Central Poland]

67%
Janczyk-Kopikowa Z., Zarski M.
Acta Palaeobotanica
|
1995
|
tom 35
|
nr 1
14

Caledonian basement [Hecla Hoek Succession] at Midterhuken, Bellsund, Spitsbergen: a revision of lithostratigraphy and age

67%
Birkenmajer K.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
2002
|
tom 50
|
nr 2
15

Skawce Sandstone Member - a new lithostratigraphic unit of the Labowa Shale Formation [Paleocene - Eocene: Magura Nappe, Siary Subunit] Polish Outer Carpathians

67%
Cieszkowski M., Waskowska-Oliwa A.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
2001
|
tom 49
|
nr 2
16

Late Carboniferous tectonic development of the Upper Silesian Coal Basin - inferred from analysis of joining

59%
Tokarski A. K., Rauch M.
Prace Naukowe Uniwersytetu Śląskiego w Katowicach
|
1996
|
nr 1602
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