Zechstein PZ3/PZ4 cyclothems boundary in the …
Three decades ago in the exposures of the Inowrocław "Solno" salt mine, mud cracks at the top of Brown Zuber complex (Na3t) of the PZ3 Zechstein cyclothem were …
Zechstein PZ3/PZ4 cyclothems boundary in the …
the top of Brown Zuber complex (Na3t) of the PZ3 Zechstein cyclothem were observed and docu-mented in photographs. Brown Zuber complex is covered by the layer of Underlying Halite which is ... Key words: Inowroc³aw, salt dome, Zechstein, PZ3/PZ4 boundary, stratigraphic discontinuity, mud cracks 283 GEOLOGIA 2011 Tom37 Zeszyt2 283–292. …
The Formation and Structure Evolution of Zechstein (Upper …
The Zechstein (Upper Permian) salts are extensively distributed in the Northeast German Basin (NEGB). ... "Fluid-Rock Interactions in the Salt Dome Environment: An Introduction and Review," Chemical Geology, Vol. 74, No. 1, 1988, pp. 1-24. ... [Upper Permian] Salt Deposits of PZ3 [Leine] Cycle in Poland," Bulletin of the Polish Academy of ...
Trace Elements and Mineralogy of Upper Permian …
Most analysed trace elements in the Zechstein potash-bearing deposits show a low content (up to 26 mg/kg) that eliminates them as potential profitable source rocks …
Zechstein PZ3/PZ4 cyclothems boundary in the Inowrocław salt dome
Three decades ago in the exposures of the Inowrocław "Solno" salt mine, mud cracks at the top of Brown Zuber complex (Na3t) of the PZ3 Zechstein cyclothem were observed and documented in photographs. Brown Zuber complex is covered by the layer of Underlying Halite which is the first member of the PZ4 Zechstein sequence. The contact …
Granica pięter cechsztynu PZ3 i PZ4 w wysadzie solnym
Na odsłonięciach w kopalni "Solno" w Inowrocławiu (obecnie zlikwidowanej) na początku lat 80. ubiegłego wieku udokumentowano fotograficznie spękania błotne na stropie zubru brunatnego Na3t kończącego cykl sedymentacyjny piętra cechsztynu PZ3. Zuber brunatny przykryty jest warstwą soli podścielającej Na4a0, która stanowi pierwszy utwór kolejnego …
(PDF) Paleofacje i paleomorfologia górnopermskich …
salt dome pierced. through Mesozoic cover. 7 Zarys budowy geologicznej. ... PZ3 (Leine, Zechstein) T1. T2 i utwory młodsze. T2 and younger deposits. PZ4 (Aller, Zechstein) NW SE. 0 5000 10000 ...
Mineralogy and geochemistry of the Tonmittelsalz (z3TM) …
Two main lithostratigraphic units of clay-bearing rock salt, the Tonmittelsalz of the Leine formation (z3) and Tonbrockensalz of the Aller formation (z4), occur in the German …
Ev i dence of high-t em per a tur e rock salt trans for ma …
The min er als and evaporite rocks within salt dome struc - tures ar e com monly so strongly trans formed t hat their com po si - tion is dif fer ent fr om their orig i nal one, ow ing to sea w a ...
Zechstein Main Dolomite oil characteristics in the
Geochemical analyses were used to classify 39 Zechstein (Late Permian, Lopingian) Main Dolomite (Ca2) crude oil samples from fields in the eastern and southern sector of the Southern Permian Basin (SPB) of Europe and to provide new insights into the origin of the oil.Geochemical data indicate that Ca2 oils were generated in the early-to …
Zechstein
The Zechstein transgression as well as the earlier marine ingressions during the Rotliegend deposition ( Legler & Schneider, 2008) have been caused by tectonic activity of the …
(PDF) Palaeogeographic and palaeoclimate factors of salinity
A study of the bromine content and facies in the salt successions (representing PZ1, PZ2 and PZ3 cycles) from the Late Permian (Zechstein) salt basin in Poland evidences fluctuations in mother ...
(PDF) Depositional conditions and paleoenvironments of the zechstein …
The limestone-marl sequence with the underlying Basal Limestone (micritic limestone) and overlying middle Zechstein (micro-oncolitic limestone) are equivalent to the carbonate rocks of the first ...
Possibility of sequence stratigraphic subdivison of the Zechstein …
Location of selected boreholes on the map of palaeo facies and palaeothicknesses of the Zechstein 4 (PZ4) in the Polish Zechstein Basin (after R. Wagner, 1994) 1-areas of erosion, 2-clastic facies ...
(PDF) Inclusions in anhydrite crystals from blue halite veins …
most Zechstein cyclothem PZ1 is know n only as tec toni cally trans ported blocks ( Charysz, 1973; Burliga et al., 1995 ). The in ter nal struc ture of the K³ odawa Salt Dome is com pli -
zechstein pz3 dome
Zechstein PZ3/PZ4 cyclothems boundary in the Inowroc³aw 31st IAS Meeting of Sedimentology studyres. Zechstein PZ3/PZ4 cyclothems boundary in the Inowroc³aw salt dome according to archival photographs of the "Solno" mine an interpretation of local sedimentation conditions in the central part of the Polish Zechstein Basin Katarzyna …
(PDF) Zechstein marine deposits in the Wleń Graben (North …
Location of the present-day Wleń Graben in relation to the original extent of the PZ3 and PZ1 cyclothems in the Polish Zechstein Basin (modi ed after W agner et al ., 1980; W agner, 1994).
zechstein pz3 dome Mar
zechstein pz3 dome Mar Impact of the Environmental Stress on the Late Permian At the end of the Permian area of Poland was an eastern margin of the epicontinental Central European Basin, called also the Zechstein Basin (Fig. 3.1a), where the cyclic sedimentation of the shallow water deposits took place.Each of the four cyclothems (PZ1–PZ4 ...
Distribution of stratiform Permian rock salt and potash
A study of the bromine content and facies in the salt successions (representing PZ1, PZ2 and PZ3 cycles) from the Late Permian (Zechstein) salt basin in Poland evidences fluctuations in mother ...
(PDF) Rozwój sedymentacji utworów ewaporatowych …
Distribution of Zechstein PZ3 cyclotheme deposits in the ar ea of Mazovia-Lublin Graben and its surrounding imaged by a set of geological sections generated from 3D model (sections location on Fig ...
Warsaw (abbreviated IG).
In the Polish part of the Zechstein basin, like in its other Central European parts, four sedimentary cycles have been recognized. The three lower ones (PZ1-PZ3) are of carbonate-evaporatic nature, the fourth one (PZ4) is clastic-evaporatic (Wagner et al. 1978). It has been found that microfauna in Zechstein carbonates is irre-
New stratigraphic scheme for Zechstein rocks in the …
Zechstein is significantly thinner than in the adjacent areas. In the Pogorzela–1 and Pogorze-la–2 wells the Zechstein is only 134 m and 85.5 m thick, whereas ... with the PZ3 cyclothem salt member also absent in the Pogo-rzela–1 and Pogorzela–2 wells. Notably, only a single carbonate
View of Zechstein PZ3/PZ4 cyclothems boundary in …
Return to Article Details Zechstein PZ3/PZ4 cyclothems boundary in the Inowrocław salt dome according to archival photographs of the "Solno" mine - an interpretation of local …
Comprehensive stratigraphic sections of the Zechstein …
Download scientific diagram | Comprehensive stratigraphic sections of the Zechstein deposits at the Golejów (loc. 1) and Wleń (loc. 2, 3) localities. Sedimentological features observed within ...
Zechstein PZ3/PZ4 cyclothems boundary in the …
Abstract: Three decades ago in the exposures of the Inowroc3aw "Solno" salt mine, mud cracks at the top of Brown Zuber complex (Na3t) of the PZ3 Zechstein cyclothem were …
Trace Elements and Mineralogy of Upper …
The potash-bearing series of PZ3 cyclothem in the Damasławek dome is represented by the Younger Potash (K3) deposits ca. 8.5–10 m thick, twice repeated in the Damasławek A borehole profile (four samples; Figure 6). They are tectonically squeezed in rock salts of the Older Halite (Na2) and sulphates of the Main Anhydrite (A3).
Impact of the Environmental Stress on the Late Permian
At the end of the Permian area of Poland was an eastern margin of the epicontinental Central European Basin, called also the Zechstein Basin (Fig. 3.1a), where the cyclic sedimentation of the shallow water deposits took place.Each of the four cyclothems (PZ1–PZ4; Fig. 3.3) began with marine carbonates and, through evaporitic …
Zechstein stratigraphy in Poland. | Download …
In contrast to the PZ1-PZ3 cycles that consist of evaporites and carbonates, the PZ4 cycle is composed of evaporites and fine siliciclastic deposits (Fig. 5) controlled by short-term climatic ...
Zechstein saline brines in Poland, evidence of
Bromine concentrations in halite, sulfate isotopes (δ 34 S and δ 18 O), and major ion concentrations in primary fluid inclusions from three boreholes in the Late Permian Zechstein evaporites have revealed sharp variations in marine derived brines within the Polish sector of the European Southern Permian Basin. The base of the Older Halite …
Geology, geochemistry and petrological
Analysis of archive and published geological, geochemical and petrological data on com- position of potash-bearing units (Older Potash (K2) and Younger Potash (K3)) of the Polish Zechstein (Late Permian) sections (mainly sampled proo les form three salt diapirs located in central Poland: Gora, K· odawa, Mogilno, and additionally for petrology from Inowroc· …
Zechstein saline brines in Poland, evidence of
This study reveals marine inputs into the Polish Zechstein Basin during deposition of the PZ1 (Werra), PZ3 (Leine), and PZ4 (Aller) cycles similar to those …
Insight Into a Shape of Salt Storage Caverns
Abstract and Figures. Salt caverns are used for over 70 years to store power sources and dispose of industrial wastes. The design of cavern shape and dimensions is still considered as a difficult ...
Quaternary subrosion and transformation of Stassfurt potash …
The dome consists of salt layers of cycles 2, 3, and 4 (z2-z4) of the Zechstein. Above-ground studies have been conducted since 1979 to determine whether the Gorleben salt dome is suited for the permanent disposal of radioactive waste. During the Elster glacial stage, the Gorleben salt dome was covered by up to 1000 m-thick ice.
SE
Zechstein units range in thickness from thin (< 50 m) or below seismic resolution in the central part of the study area, to extreme local maxima (> 3000 m) in diapiric structures in the southern (Salt Dome Province) and very northwestern parts (Figs. 5e–f, 9). Zechstein deposits are absent where the Top pre-Zechstein is the shallowest …
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