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23篇 您的检索式:作者名="Krystyn"
    题名 作者 年代 出处 被引量
1Triassic pelagic deposits of Timor: palaeogeographic and sea-level implications显示文摘R Martini L Zaninetti M Villeneuve J.-J Cornée L Krystyn S Cirilli P De Wever P Dumitrica A Harsolumakso 2000Palaeogeography Palaeoclimatology Palaeoecology2000,,1:1
2SJES14110600031473显示文摘Matthew J. Whitfield David Bono Lei Wei Krystyn J. Van Vliet 2014Corrosion Science2014,,:1
3Contact Creep Compliance of Viscoelastic Materials via Nanoindentation显示文摘Tweedie Catherine A Krystyn J 2006Journal of Materials Research2006,6,6:1
4Termination of carbonate slope progradation:an example from the Carnian of the Dolomites,Northern Italy显示文摘KEIM L BRANDNER R KRYSTYN L 2001Sed Geol2001,143,:1
5Sequencing events across the Permian–Triassic boundary, Guryul Ravine (Kashmir, India)显示文摘Thomas J. Algeo Robyn Hannigan Harry Rowe Michael Brookfield Aymon Baud Leo Krystyn Brooks B. Ellwood 2007Palaeogeography Palaeoclimatology Palaeoecology2007,,1:1
6Evaluation of the in- fluence of exposure to tobacco smoke on the concentration of the preg- nancy-associated plasma protein A in the population of healthy men and non-pregnant women显示文摘Szumska M Krystyn'a T Wielkoszyflski T 2013Przegl Lek2013,70,10:1
7A Tethys-wide mid-Carnian (Upper Triassic) carbonate productivity crisis:Evidence for the Alpine Reingraben Event from Spiti (Indian Himalaya)?显示文摘HORNUNG T KRYSTYN L BRANDNER R 2007Journal of Asian Earth Sciences2007,30,:1
8Permian-Triassic boundary interval in the Middle East (Iran and N Oman) : progressive environmental change from detailed carbonate carbon isotope marine curve and sedimentary evolution 显示文摘Riehoz S Krystyn L Baud A 2010Journal of Asian Earth Sciences2010,39,4:1
9The Rhaetian stage-chronostratigraphy,subdivisions and their intercontinental correlation显示文摘Krystyn L 1990Albertiana1990,8,:1
10Boundary-integral approach to determine the magnetic field created by a permanent magnet put in free space显示文摘Krystyn Pawluk Zdzislaw Zycki 2000Compel2000,19,1:1
11Termination of carbonate slope progradation:An example from the Carnian of the Dolomites,northern Italy显示文摘Lorenz Keim Rainer Brandner Leopold Krystyn 2001Sedimentary Geology2001,143,:1
12Mechanical Resuscitation of Chemical Oscillations in Belousov–Zhabotinsky Gels显示文摘Irene Chou Chen Olga Kuksenok Victor V. Yashin Anna C. Balazs Krystyn J. Van Vliet 2012Adv Funct Mater2012,,12:1
13The role of laparoscopy in abdominal trauma - review of the literature 显示文摘Maciej W Krystyn S Jerzy P 2011Wideochir Inne Tech Malo Inwazyjne2011,6,3:1
14Size effects on the onset of plastic deformation during nanoindentation of thin films and patterned lines显示文摘Choi Yoonjoon Van Vliet Krystyn J Li Ju 2003J Appl Phys2003,94,9:1
15Western Tethyan Epeiric Ramp Setting in the Early Triassic: An Example from the Central Dinarides (Croatia)显示文摘In the central part of the External Dinarides in Plavno, Croatia, near Knin, a remarkably thick(927.5 m) Early Triassic depositional sequence was investigated. The Plavno sequence starts in the Early Griesbachian and ends with a continuous transition into the Anisian strata. A complete 13 C isotope curve has been achieved and combined with conodonts, bivalves and ammonoids to establish and correlate stage and substage boundaries. The δ13 C curve is consistent with former studies. It displays a general increase from the Griesbachian to a prominent maximum beyond the +8‰ amplitude around the Dienerian-Smithian boundary(DSB), followed by a steep and continuous decline to low, negative values in the Smithian. Around the Smithian-Spathian boundary(SSB) a steep rise to a second maximum occurred. It is followed by a saw-tooth shaped decline in the Spathian and a similar increase to a peak at the Spathian-Anisian boundary(SAB). Sedimentologically, the Plavno sequence is interpreted as having been deposited on an extensive epeiric ramp under long-term transgressive conditions, sharing depositional characteristics of both the epeiric platform and the carbonate ramp. The entire Plavno sequence was deposited above the storm-wave base and was storm influenced. Three informal members are differentiated: 1) the dolostone member(Early Griesbachian); 2) the siliciclastic member(red-coloured shale, siltstone, sandstone with oolitic/bioclastic grainstone intercalations), which can be further divided into lower, middle and upper intervals(Late Griesbachian, Dienerian and Smithian); and 3) the mudstone member(grey lime mudstones, marls and calcisiltites with common ammonoids and gastropods-Spathian). The Plavno sequence is compared with other western Tethyan sections. Observed differences stem from local controls on deposition in the overall shallow marine environment.Dunja Aljinovic Micha Horacek Leopold Krystyn Sylvain Richoz Tea Kolar-Jurkovsek Duje Smircic Bogdan Jurkovsek 2018Journal of Earth Science2018,29,4:1
16Termination of carbonate slope progradation:an example from the Carnian of the Dolomites,Northern Italy显示文摘Keim L Brandner R Krystyn L Mette W 2001Sedimentary Geology2001,,143:1
17Total merit index to estimate the breeding value of polish arctic foxes显示文摘Heliodor W Boleslaw Z Krystyn C 2006Animal Science Papers and Reports2006,24,2:1
18Compositional dependence of Young's moduli for amorphous Cu-Zr films measured using combinatorial deposition on microscale cantilever arrays 显示文摘GUO Qiang ZHANG Li ZEIGER ADAM S LI Yi Van VLIET KRYSTYN J THOMPSON CARL V 2011Scripta Materialia2011,64,1:1
19Rapid marine recovery after the end-Permian mass-extinction event in the absence of marine anoxia显示文摘Twitchett R J Krystyn L Baud A 2004Geology2004,32,:1
20Differential regulation of BACE1 promoter activity by nuclear factor-B in neurons and glia upon exposure to - amyloid peptides显示文摘Krystyn Z Bourne 2007J Neurosci Res2007,85,:1
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