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| 1 | Palaeogeographical zonation of gypsum facies:Middle Miocene Badenian of Central Paratethys (Carpathian Foredeep in Europe)显示文摘Studies on Middle Miocene Badenian gypsum in various parts of Central Paratethys,the oldest widespread primary marine gypsum,in western Ukraine,southern Poland and Moravia (Czech Republic) indicate that there are three principal gypsum facies:crystalline gypsum,stromatolitic gypsum and clastic gypsum.The latter typically occurs between crystalline and stromatolitic gypsum and between stromatolitic gypsum and the land.In addition,it is common in channels within gypsum microbialites,and is the main facies during the deposition of the upper part of Badenian gypsum when important bathymetric differences existed within the marginal part of the Carpathian Foredeep Basin,the largest foredeep basin in Europe.Within crystalline gypsum facies,it is observed the overall size of the crystals increases and that the layering declines towards the permanent,stabilized brine body,and thus the giant gypsum intergrowths-non-layered coarse-crystalline selenite is the end-member of gypsum facies continuum.Typically it passes into layered selenites although owing to fluctuations of pycnocline level,some transitional gypsum subfacies may be missing both in the vertical section as well as in particular outcrops.The following important controls on the development of gypsum facies have been identified:pycnocline level fluctuations,brine level fluctuations including brine sheets and floods,rare marine transgressions,pedogenesis leading to 'alabastrine' gypsum development,and rate of inflow of continental water. | Tadeusz Marek Peryt | 2013 | Journal of Palaeogeography2013，2，3： | 2 |
| 2 | Stable chlorine isotopes in Phanerozoic evaporites显示文摘 | C.J. Eastoe T.M. Peryt Oleh Y. Petrychenko D. Geisler-Cussey | 2006 | Applied Geochemistry2006，，3： | 1 |
| 3 | Origin ofpolyhalit e deposit s in theZechstein ( Upper Permian) Zdrada plat form ( northern Poland ) 显示文摘 | Peryt Pierre and Gryn iv | 1998 | Sediment ology1998，45，3： | 1 |
| 4 | Marine and continental lower permian evaporites of the Prypiac' Trough (Belarus) 显示文摘 | Vysotskiy E A Makhnach A A Peryt T M | 2004 | Sedimentary Geology2004，172，12： | 1 |
| 5 | Sedimentary and environmental history of the Late Permian Bonikowo Reef(Zechstein Limestone, Wuchiapingian), western Poland显示文摘The Bonikowo Reef occurs in the central part of the Zechstein Limestone Basin in western Poland and was growing on the topmost edges of tilted blocks and/or on the top of uplifted horsts of the BrandenburgeWolsztynePogorzela High. Its size is ca. 1.6 km2. The Bonikowo Reef shows the thickest reef section(90.5 m) recorded in the High. The Zechstein Limestone unit is represented mostly by limestones, often thoroughly recrystallized, although the macrotextures and biota of the boundstone are identifiable in most cases. The drillcore section is a mixture of boundstones(microbial and bryozoan), wackestones, packstones and grainstones, which often co-occur. The d13 C and d18 O values for both calcite(avg. 3.8 ± 0.8‰ and-3.4 ± 1.7‰, respectively) and dolomite(avg. 3.5 ± 0.7‰ and-5.2 ± 1.3‰, respectively) are transitional between the values previously reported for condensed sequences of the basinal facies and larger reef complexes. The biofacies of the Bonikowo Reef are very similar to those recognized in other reefs of the BrandenburgeWolsztynePogorzela High, which owe their origin to the destruction of bryozoan boundstones. The biota composition is typical and characteristic of other Zechstein Limestone reefs. However, the Bonikowo Reef demonstrates the importance of microbialites, laminar and nodose encrustations, in the growth and cohesion of the Zechstein Limestone reefs. Such encrustations abound within the Zechstein Limestone although, in many cases, the real nature of the encrustations is difficult to ascertain. These laminated encrustations show great similarity to Archaeolithoporella that is one of the most important Permian reefbuilding organisms. The encrustations considered to represent Archaeolithoporella were also previously recorded in the Zechstein Limestone of western Poland and in its stratigraphic equivalent, the Middle Magnesian Limestone of Northeast England. The lower part of the sequence shows great biofacies variability that reflects common environmental changes. The major part of the section is represented by slope depositsgrading upward into the reef, which reflects the prograding nature of reef margin. The progradation rate for the Bonikowo Reef is estimated at 400 m/My. | Pawe? Raczyński Tadeusz Marek Peryt Wac?aw Strobel | 2017 | Journal of Palaeogeography2017，6，3： | 1 |
| 6 | Stable chlorine isotopes in Phanerozoic evaporates 显示文摘 | Eastoe C J Peryt T M Petrychenko O Y | 2007 | Applied C eochemistry2007，22，3： | 1 |
| 7 | Seawater composition during deposition of visean evaporates in the Moncton sub-basin of new Brunswick as inferred from the fluid inclusion study of halite 显示文摘 | Petrychenko O Peryt T M Roulston B | 2002 | Canada Journal of Earth Sciences2002，39，2： | 1 |
| 8 | Secular varia- tion in seawater chemistry during the Phanerozoic as indica- ted by brine inclusions in halite 显示文摘 | Kovalevich V M Peryt T M Petrichenko O I | 1998 | The Journal of Geolo- gy1998，106，： | 1 |
| 9 | Seawater composition during deposition of visean evaporites in the Moncton sub- basin of new Brunswick as inferred from the fluid inclusion study of halite 显示文摘 | Petrychenko O Peryt T M Roulston B | 2002 | Canadia Journal Earth Sciences2002，39，2： | 1 |
| 10 | Changes of sea- water composition in the Triassic-Jurassic time as recorded by fluid inclusions in halite 显示文摘 | Khmelevska O Kovalevych V Peryt T M | 2000 | Journal of Geochemical Ex- ploration2000，8386，： | 1 |
| 11 | Secular Variation in Seawater Chemistry during the Phanerozoic as Indicated by Brine Inclusions in Halite显示文摘 | Kovalevich V M Peryt T M Petrichenko 0 I | 1998 | The Journal of Geology1998，106，： | 1 |
| 12 | Demise of the Jablonna Reef(Zechstein Limestone)and the onset of gypsum deposition(Wuchiapingian,west Poland):carbonate-to-evaporite transition in a saline giant显示文摘Microbial deposits commonly occur at the transition between carbonate and sulphate facies,and they also abound in the uppermost part of the middle Wuchiapingian Zechstein Limestone in west Poland.These deposits occur as isolated reefs of the basinal zone and in the condensed sequences in most parts of the study area.The deposits of the latter category reflect evaporative drawdown,and the abrupt boundary between the carbonate and sulphate deposits in the basin suggests the nature of evaporites that start to precipitate as soon as they reach the saturation level.A few-metre-thick unit of mostly brecciated microbial deposits at the top,reefal portion of the Zechstein Limestone records extreme palaeoenvironmental events that occurred at the transition from carbonate to sulphate deposition.These events are related first to subaerial exposure of the reef,which lasted several 10~5 years and then to the Lower Anhydrite transgression. | Tadeusz Marek Peryt Marek Jasionowski Pawet Raczyiiski Krzysztof Chtdek | 2020 | Journal of Palaeogeography2020，9，3： | 1 |
| 13 | Origin of polyhalite deposits in the Zeehetein( Upper Perm Jan) Zdrada plat form (northern Poland) 显示文摘 | Peryt Pierre and Gryn iv | 1998 | Sediment ology1998，45，3： | 1 |
| 14 | The Cenomanian-Turonian oceanic anoxic event in SE Poland显示文摘 | Peryt D Wyrwicka K | 1991 | Cretaceous Research1991，12，： | 1 |
| 15 | Chemical composition of seawater in Neoproterozoic: Results of fluid inclusion study of halite from Salt Range (Pakistan) and Amadeus Basin (Australia) 显示文摘 | KOVALEVYCH V M MARSHALL T Peryt T M | 2006 | Precambrian Research2006，144，： | 1 |
| 16 | Chemical composition of seawater in Neoproterozoic:Results of fluid inclusion study of halite from salt range(Pakistan)and Amadeus Basin(Australia)显示文摘 | Kovalevych V M Marshall T Peryt T M | 2006 | Precambrian Research2006，144，： | 1 |
| 17 | Ground Vibration Generated by a Harmonic Load Acting on a Railway Track显示文摘 | Sheng X Jones C J C Peryt M | 1999 | Journal of Sound and Vibration1999，225，1： | 1 |
| 18 | Mechanism of antimutagenicity of wheat sprout exacts 显示文摘 | Peryt B Szymczyk T Lesca P | 1992 | Murat Res1992，269，： | 1 |
| 19 | Possibility of sequence stratigraphic subdivi- sion of the Zechstein in the Polish Basin显示文摘 | Wagner R Peryt T M | 2013 | Geological Quarterly2013，41，4： | 1 |
| 20 | Chemical compo- sition of seawater in Neoproterozoic: Results of fluid inclusion study of halite from Salt Range (Pakistan) and Amadeus Basin (Australia) 显示文摘 | Kovalevych V M Marshall T Peryt T M | 2006 | Precambrian Research2006，144，1： | 1 |
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