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1

Gosau-type conglomerate in the Rusinowa Polana Area, Polish Tatra Mts: its relation to the Lower Subtatric Nappe

100%
Birkenmajer K.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
2000
|
tom 48
|
nr 1
2

The Margot Formation in Western Cuba: a volcanic and sedimentary sequence of [Mainly] Cenomanian-Turonian age

84%
Pszczolkowski A.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
2002
|
tom 50
|
nr 2
3

Models of deformation in sedimentary rocks

84%
Pininska J.
Prace Naukowe Uniwersytetu Śląskiego w Katowicach
|
1996
|
nr 1602
4

Faulting of a foliated rock in a general triaxial field of compressive stresses

84%
Kwasniewski M. A., Mogi K.
Prace Naukowe Uniwersytetu Śląskiego w Katowicach
|
1996
|
nr 1602
5

Cuesta landscape in the middle part of the Sudetes Mts

84%
Tulaczyk S.
Geographia Polonica
|
1992
|
tom 60
6

Warsaw ING PAN Isotope Laboratory research reports. 3. Recrystallization of belemnite rostra and its bearing on Sr isotopic ratios

67%
Zielinski G.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
1998
|
tom 46
|
nr 2
7
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Palaeoecology of free-lying domal bryozoan colonies from the Upper Eocene of Southeastern USA

67%
McKinney F. K., Taylor P. D.
Acta Palaeontologica Polonica
|
2003
|
tom 48
|
nr 3
Dome−shaped cheilostome bryozoan colonies, most commonly about 2 cm in diameter, are common in Upper Eocene offshore deposits of southeastern North Carolina, USA.This colony−form is anachronistic in the Eocene, being more typical of Palaeozoic bryozoans.There are three types of domes: individual colonies of Parasmittina collum (Canu and Bassler), individual colonies of Osthimosia glomerata (Gabb and Horn) and multispecies intergrowths.The bryozoans grew laterally beyond initial shell substrata to become free−lying. P. collum colonies grew by local eruptive budding, forming subcolonies that extended radially over the underlying layer of zooids.Undersides of subcolonies that extended beyond the original substratum have basal exterior walls that are more commonly fouled by encrusters than is the upper side of the colony.By contrast, lateral growth of O. glomerata colonies was limited by size of the original substratum, subcolonies were not developed, and colony growth occurred by prolific frontal budding over the entire upper surface of the colony. Undersides of colonies beyond the substratum consist of the lateral interior walls of marginal zooids and are much less commonly fouled than are undersurfaces of P. collum.The upper surfaces of multispecies domes by definition are always fouled, and their undersurfaces are also commonly fouled.
8

Characterization of opoka as a basis for its use in wastewater treatment

67%
Brogowski Z., Renman G.
Polish Journal of Environmental Studies
|
2004
|
tom 13
|
nr 1
Opoka, as a silica-calcite sedimentary rock, occurs in south-eastern Europe and Russia. Stratigraphical studies down to 8 m depth were performed in Bełżec, Poland, where samples were taken for further analyses. Vertical layers represented a heavy-weight opoka consisting of relatively more CaCO3 than the horizontal layers of lightweight opoka dominated by SiO2 . Opoka had a mean bulk density of 1.34 g/cm3, a porosity of 44.5 % and a specific surface area of 64 m2 /g. Opoka, especially after heated to over 900℃ can be used as reactive filter media for phosphorus removal. Maximum sorption capacity was 119.6 g PO4 -P/ kg. Element analysis of the rock did not reveal any anomaly from that expected, and it was concluded that its element content does not devaluate opoka as a sorbent used in ecological wastewater treatment .
9

Pre-glacial sedimentary facies of the Point Thomas Formation (Eocene) at Cytadela, Admiralty Bay, King George Island, West Antarctica

59%
Mozer A.
Polish Polar Research
|
2012
|
tom 33
|
nr 1
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