Biuletyn Państwowego Instytutu Geologicznego最新文献_第3页

HOLOCENE EVOLUTION OF THE PEAT-BOG IN SŁUPIAŃSKA BAY (WIGRY LAKE, NE POLAND) IN THE LIGHT OF MALACOLOGICAL ANALYSIS 波兰sŁupiaŃska湾(wigry lake, ne poland)泥炭沼泽的全新世演化

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2018-12-20 DOI: 10.5604/01.3001.0012.7706

W. Alexandrowicz, S. Żurek

{"title":"HOLOCENE EVOLUTION OF THE PEAT-BOG IN SŁUPIAŃSKA BAY (WIGRY LAKE, NE POLAND) IN THE LIGHT OF MALACOLOGICAL ANALYSIS","authors":"W. Alexandrowicz, S. Żurek","doi":"10.5604/01.3001.0012.7706","DOIUrl":"https://doi.org/10.5604/01.3001.0012.7706","url":null,"abstract":"Three types of molluscan assemblages have been identified in a profile of calcareous gyttja and peat penetrated by drilling within the raised peat-bog of the Słupiańska Bay. Numerous shells of molluscs have been identified within the 5.35 m thick intervals of fine detritus of the calcareous gyttja. The shells belonged primarily to the bivalves and water snails. Terrigenous species appeared only rarely and have been more frequent in the upper part of the penetrated interval. The three distinguished molluscan assemblages have been described and interpreted in terms of representing different environmental conditions. Assemblage with Gyraulus laevis that occurs within the lower part of the interval consists of the cold-loving forms representing early Holocene. Assemblage with Gyraulus albus that occurs in the middle part of the interval consists of warm-loving species linked to the Atlantic Phase. Assemblage with terrigenous species, mainly snails, occurs in the upper part of the interval. The distinguished types of molluscan assemblages are composed of species characteristic of littoral habitat of ephemeral lakes and some of terrestrial habitats. Lake-level fluctuations are expressed by changing of molluscan fauna. Variable proportions of Bithynia tentaculata shells and opercula indicates low-level water stages of the Wigry Lake that took place during the Boreal Phase, the middle part of the Atlantic Phase and during the termination of the Sub Boreal and Sub Atlantic phases. The completion of gyttja accumulation and the beginning of peat deposition are associated with the latter period.\u0000\u0000","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-12-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"130893765","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 2

SIGNIFICANCE OF THE ROAD-CUTS AND OTHER ROCK SECTIONS EXPOSED BY THE NEW LINEAR INVESTMENTS FOR THE GEOLOGICAL RESEARCH IN POLAND 新的线性投资暴露的道路切割和其他岩石剖面对波兰地质研究的意义

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2018-12-20 DOI: 10.5604/01.3001.0012.7712

Krzysztof Urbański

引用次数: 0

LANDSLIDES AND THE INCORRECT INTERPRETATION OF GEOLOGICAL STRUCTURE – EXAMPLES FROM THE SUDETY MOUNTAINS 滑坡和对地质构造的错误解释——以苏迪特山脉为例

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2018-12-20 DOI: 10.5604/01.3001.0012.7708

A. Kowalski

引用次数: 4

VARIATIONS IN THE AMOUNT OF MINERAL RESOURCES AND MINING PRODUCTION OF POLAND AFTER WORLD WAR II 第二次世界大战后波兰矿产资源和采矿产量的变化

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2018-12-20 DOI: 10.5604/01.3001.0012.7710

W. Salski

引用次数: 0

SOIL CONTAMINATION INDUCED BY HISTORICAL ZINC-LEAD ORE MINING AND IRON AND ZINC SMELTING IN THE CENTRAL PART OF THE UPPER SILESIAN INDUSTRIAL REGION (SOUTHERN POLAND) 上西里西亚工业区中部(波兰南部)历史铅锌矿开采和铁锌冶炼引起的土壤污染

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2018-12-20 DOI: 10.5604/01.3001.0012.7709

A. Pasieczna

引用次数: 0

Application of the portable spectrometer XRF for the determination of content of some metals in soil: A case study from Holy Cross Mountains (Central Poland) 便携式XRF光谱仪在土壤中某些金属含量测定中的应用——以圣十字山(波兰中部)为例

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2018-11-20 DOI: 10.5604/01.3001.0012.7121

P. Kuc, P. Lenik, J. Bazarnik

{"title":"Application of the portable spectrometer XRF for the determination of content of some metals in soil: A case study from Holy Cross Mountains (Central Poland)","authors":"P. Kuc, P. Lenik, J. Bazarnik","doi":"10.5604/01.3001.0012.7121","DOIUrl":"https://doi.org/10.5604/01.3001.0012.7121","url":null,"abstract":"The analysis of chemical composition using the portable X-ray fluorescence spectrometer (p-XRF) is recently rapidly developing instrumental research method. This method was applied to analyze the content of selected elements in soil samples from the Strużna region of the Holy Cross Mountains. The Olympus Delta Premium p-XRF spectrometer (4W Ta anode X ray tube, 40 kV, 200 μA current beam, “soil” mode, 135 seconds) was used. Prior to analyze the soil samples, the NIST 2710a and NIST 2711a reference standards were utilized in order to calibrate the p-XRF spectrometer. The maps showing obtained results of K, Ca, Fe, Mn, Cu, Zn, As and Pb were constructed using the SURFER 7.0 software with kriging procedure. The obtained results show arithmetic means similar to the previously obtained using traditional methods of chemical analysis for the soils of Holy Cross Mountains. These results combined with the high accuracy of measurements obtained by using the p-XRF Olympus Delta X spectrometer proved this device to be the effective tool for environmental and geochemical studies.\u0000\u0000","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"10 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-11-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"128693955","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Geological setting of the barite-fluorite deposit at Jeżów Sudecki (Kaczawa Mts.) Jeżów Sudecki (Kaczawa山)重晶石萤石矿床地质背景

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2018-11-20 DOI: 10.5604/01.3001.0012.7120

Cezary Sroga, W. Bobiński, W. Kozdrój

{"title":"Geological setting of the barite-fluorite deposit at Jeżów Sudecki (Kaczawa Mts.)","authors":"Cezary Sroga, W. Bobiński, W. Kozdrój","doi":"10.5604/01.3001.0012.7120","DOIUrl":"https://doi.org/10.5604/01.3001.0012.7120","url":null,"abstract":"From 1969 to 1993, investigation for the Ba-F mineralization was executed within the metamorphic Kaczawa complex, north of the Intra-Sudetic Fault in the Jeżów Sudecki-Dziwiszów area (Kaczawa Mts., Western Sudetes). The article presents unpublished results of those prospecting works. A small deposit of Ba-F with Zn, Pb, Cu-sulphides, on the SE slope of the Szybowisko hill near Jelenia Góra, was documented in 1994. The economic mineralization is developed in the Jeżów Sudecki fault, steep fracture zone running parallel to the Intra-Sudetic Fault, and was identified at a distance of 600 m along the strike of the fault (in the W–E direction) and up to a depth of 500 m along the dip (towards the south). Two (locally three) bifurcating veins were found. The average content of the main components is: BaSO4 – 63.18%, CaF2 – 8.60%. The Ba-F mineralization is associated with the Jeżów Sudecki fault, synchronous with the formation of the Intra-Sudetic Fault zone. Both of these faults are Variscan and fall steeply southward. Younger, alpine (?) inverse and transverse normal faults were formed after the intrusion of a rhyolite dyke into the Kaczawa complex rocks and after the formation of the barite deposit. The Ba-F mineralization developed in a multi-stage process and shows a pulsatory nature. Five mineral parageneses were distinguished in the deposit. The age of the Ba-F mineralization has not been definitively established.\u0000\u0000","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"40 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-11-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"129859943","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 3

Odnawianie się rozsypisk złotonośnych przedpola Sudetów Wschodnich

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2018-11-20 DOI: 10.5604/01.3001.0012.7119

J. Wierchowiec

{"title":"Odnawianie się rozsypisk złotonośnych przedpola Sudetów Wschodnich","authors":"J. Wierchowiec","doi":"10.5604/01.3001.0012.7119","DOIUrl":"https://doi.org/10.5604/01.3001.0012.7119","url":null,"abstract":"W obrębie sekwencji okruchowych przedpola Sudetów Wschodnich wyróżniono w sumie pięć różnowiekowych poziomów złotonośnych związanych z preglacjalnymi „białymi” żwirami typu serii Gozdnicy, wodnolodowcowymi piaskami i żwirami plejstocenu oraz osadami holoceńskich tarasów Złotego Potoku i Białej Głuchołaskiej. Maksymalne zawartości Au (0,4 g/m3 osadu) notuje się w grubookruchowych żwirach kwarcowych, przestrzennie związanych z preglacjalną (eoplejstoceńską) doliną paleo-Białej Głuchołaskiej. Na powierzchni wyróżnionych dwóch podtypów złocin (ziarna blaszkowo-płytkowe, płaskie lub wtórnie zdeformowane oraz cementacyjno-grudkowe) rozpoznano i opisano nano- i mikrostruktury (morfotypy) Au oraz wewnętrzne tekstury (widoczne w przekroju ziaren), wskazujące na procesy tzw. odnawiania się rozsypisk złotonośnych. Są one wiązane z selektywnym rozpuszczaniem złota w warunkach hipergenicznych, jego wytrącaniem z roztworu i wtórną rekrystalizacją prowadzącą w rezultacie do formowania skupień złota autogenicznego. Rozpoznano dwa morfotypy złota autogenicznego: banieczkowate lub drobnorobaczkowe skupienia Au oraz krystaliczne skupienia i przerosty złota. Wspomniane morfotypy są bardzo dobrze zachowane i nie noszą oznak abrazji. Szczegółowa analiza SEM pokazuje, że pojedyncze banieczkowate nanocząsteczki z czasem zrastały się formując inkrustacje Au, a ostatecznie warstwę złota autogenicznego na powierzchni złociny pełniącej rolę swego rodzaju osadnika dla nowych nanocząstek. Występowanie banieczkowatych lub drobnorobaczkowych skupień Au w paragenezie z minerałami ilastymi oraz brak jakichkolwiek oznak abrazji tych skupień wskazują, że utworzyły się one in situ, to jest są pochodzenia autogenicznego. Nano- i mikroskupienia złota robaczkowo-pęcherzykowego zbudowane ze złota amorficznego mogą być wynikiem koagulacji koloidów lub ich adsorpcji przez minerały ilaste wypełniające kawerny na powierzchni złocin. Krystaliczne przerosty złota są prawdopodobnie efektem rekrystalizacji złota koloidalnego wytrącanego na powierzchni złocin po depozycji w rozsypisku.\u0000\u0000","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-11-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"129962373","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Lignite deposits of the Poznań rift valleys system as a guarantee of energy security for Poland 波兹纳兹裂谷系统的褐煤矿床是波兰能源安全的保障

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2018-11-20 DOI: 10.5604/01.3001.0012.7100

P. Urbański

引用次数: 1

SAFEGUARDING OF MINERAL RAW MATERIALS DEPOSITS – A CONCEPT OF VALORIZATION AND SELECTION OF MINERAL DEPOSITS OF PUBLIC IMPORTANCE 矿物原料矿床的保护-对公众重要的矿床进行估价和选择的概念

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2018-11-20 DOI: 10.5604/01.3001.0012.7098

Stanisław Wołkowicz, Olimipa Kozłowska, K. Andrzejewska-Kubrak, D. Brzeziński

{"title":"SAFEGUARDING OF MINERAL RAW MATERIALS DEPOSITS – A CONCEPT OF VALORIZATION AND SELECTION OF MINERAL DEPOSITS OF PUBLIC IMPORTANCE","authors":"Stanisław Wołkowicz, Olimipa Kozłowska, K. Andrzejewska-Kubrak, D. Brzeziński","doi":"10.5604/01.3001.0012.7098","DOIUrl":"https://doi.org/10.5604/01.3001.0012.7098","url":null,"abstract":"The article presents a proposal for the new rules for the selection of deposits, which due to their value should be protected as Mineral Deposits of Public Importance (MDoPI) on national level. It was assumed that safeguarding should cover only the largest recognized deposits in terms of resources located in areas not excluding exploitation, which meet jointly two criteria: the total resources of the largest deposits should cover at least 50% of national geological resources and simultaneously they should meet the criterion of security of supply minerals for at least 50 years, with average demand calculated based on data from the last 10 years. Using the above criteria, analysis of the following deposits was performed: gypsum and anhydrite, basalt, granite, granodiorite, erratic boulder and syenite, dolomite, marl, travertine, limestone and dolomitic limestone, quartzite, greywacke, sandstone, quartzite sandstone, marl and limestone for the cement industry as well as limestone and marl for the lime industry. In total, 828 deposits were analyzed, and the assumed criteria were fulfilled in this group of deposits by a total number of 82 deposits. Among them, 6 deposits are very conflict, 71 – conflict, and 5 – partly conflict. In the case of several very conflict deposits, there is a high probability that their exploitation will not be possible, so meeting the criteria will require extending the list of deposits by 6 other ones. It was proposed that the verification of valorisation of deposits classified as MDoPI should be carried out periodically – not more often than every 5, but not less than every 10 years. This task should belong to the duties of the geological survey.\u0000\u0000","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"122 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-11-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121952048","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 1