Actual Questions of Waterworks Biology. (in Czech), collected papers from a seminar held on February 12, 1986 in Prague,Prague, Czech Scientific-Technical Society,p. 161, not on market     

V. Slde ek 《洁净——土壤、空气、水》1989,17(1):111-111

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Actual questions of Waterworks Biology 1987. (in Czech), collected papers from a seminar held on January 15, 1987 in Prague,Prague, Czech Scientific-Technical Society, 1987, p. 183, not on market     

V. Slde ek 《洁净——土壤、空气、水》1989,17(1):112-112

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Radioactive and trace element distribution in basaltic rocks of Lower Silesia     

Vladimír Kropáček  Věra Vaňková  Reviewer J. Fiala 《Studia Geophysica et Geodaetica》1985,29(3):290-299

Summary The distribution of radioactive(Th, U, K) and selected trace(Rb, Sr, Ba, Y, Zr, V, Cr, Ni) elements in volcanic rocks from the Opole and Jawor regions of the Lower Silesia has been studied. The behaviour of these elements in the studied rocks indicates that the Lower Silesian volcanic rocks are characterized by less differentiated type than other volcanic rocks of the Bohemian Massif, the Opole rock types probably having a less differentiated character than the Jawor rock types.

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¶rt;a an¶rt;u a¶rt;uamu(Th, U, K) u m ¶rt;u(Rb, Sr, Ba, Y, Zr, V, Cr, Ni) m auu n¶rt;a am n u u uuu. a n mam n¶rt;num, m aum u uuu n¶rt;mam ¶rt; aamuu n¶rt; u ¶rt;uuau, aum u ana¶rt; uu. au a n¶rt;num, m auu n¶rt; amu n ¶rt;uuau ma ua n¶rt; u amu .

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STELLA,E.: Fondamenti di Limnologia. Guida allo studio delle acque continentali. Con la collaborazione di F. G. MARGARITORA e G. MURA. Roma,Edizioni dell' Ateneo, 1984. 300 S., 78 Abb., 26 Farbphotos, 4 schwarz-weiß Photos, 12 Tab., Lire 30.000     

V. Slde ek 《洁净——土壤、空气、水》1985,13(2):222-222

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HUBER-PESTALOZZI,G.: Das Phytoplankton des Süßwassers. Chlorophyceae (Grünalgen), Ordnung Chlorococcales,von J. KOMÁBEK und B. FOTT. Die Binnengewässer 16 (7. Teil, 1. Hälfte). Stuttgart,Schweizerbart'sche Verlagsbuchhandlung, 1983. 1044 S., 253 Abb     

V. Slde ek 《洁净——土壤、空气、水》1985,13(2):244-244

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RGW-Symposium über die technische Hydrobiologie     

V. Slde ek 《洁净——土壤、空气、水》1985,13(2):264-266

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P. M. JONASSON (Ed.): Ecology of eutrophic,subarctic Lake Mývatn and the River Laxá. — Published by the Icelandic Literature Societty ib Copenhagen, 1984, 308 S., zahlr. Abbildungen und Farbphotographien     

V. Slde ek 《洁净——土壤、空气、水》1985,13(4):488-488

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Microlaboratory study on magnetic,gravity and high-tension separation of hercynite and pleonaste from low-grade ilmenite concentrates     

Jan Drzymala  Andrzej łuszczkiewicz 《International Journal of Mineral Processing》1985,14(3):233-238

Some ilmenite concentrates obtained from oleate flotation of ilmenite ores from NE Poland contain less than the required 45% TiO₂ due to the presence of green spinels (hercynite and pleonaste). Such concentrates were further upgraded by different separation techniques. It was established at microlaboratory scale that magnetic, gravity and high-tension separations can provide qualified ilmenite concentrates with TiO₂ recovery in the order of 50 to 80%.  相似文献   

КРИТИКА     

František Anýž 《Studia Geophysica et Geodaetica》1984,28(3):321-322

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A volcanic-carbonate association in the Góry Kaczawskie,Western Sudetes     

Dr. Zdzisław Baranowski  Dr. Stanbław Lorenc 《International Journal of Earth Sciences》1986,75(3):595-599

Amidst metavolcanic rocks and phyllites of the Góry Kaczawskie region occur isolated carbonate bodies known as the Wojcieszów limestones. The bodies enclosed in the metavolcanites show primary (sedimentary) contacts, while those in the phyllites do not have such contacts. The Wojcieszów limestones and metavolcanic rocks form sequences displaying mutual spatial and genetical relations. Submarine volcanic elevations were covered with chemical and biochemical carbonate precipitation, the intensity of which was stimulated and controlled by the volcanic activity.

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Zusammenfassung Inmitten der metavulkanischen Gesteine und Phyllite von Góry Kaczawskie erscheinen isolierte Karbonatgesteinskörper, die als Wojcieszów-Kalke bekannt sind. Die Karbonatgesteine innerhalb der Metavulkanite zeigen sedimentäre Kontakte, während die in den Phylliten eher tektonisch begrenzt sind. So kann man den Wojcieszów-Kalken und den Metavulkaniten eine räumliche und genetische Beziehung zusprechen. Submarine Erhebungen aus Vulkangesteinen waren mit chemischen und biochemisch gefällten Karbonatserien bedeckt, wobei die vulkanische Aktivität die Karbonatbildung unmittelbar beeinflu\te.

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Résumé Parmi les métavolcanites et les phyllites de la région du Góry Kaczawskie, il existe des corps carbonatés isolés connus sous le nom de »calcaires de Wojcieszów«. Ceux qui sont inclus dans les métavolcanites présentent des contacts sédimentaires, contrairement à ceux qui sont inclus dans les phyllites, dont les contacts sont tectoniques. Entre les calcaires de Wojcieszów et les roches métavolcaniques, il est donc possible d'établir des relations spatiales et génétiques. Des reliefs volcaniques sous-marins ont été le siège d'une précipitation carbonatée chimique et biochimique dont l'intensité dépendait de l'activité volcanique.

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