Biuletyn Państwowego Instytutu Geologicznego最新文献_第2页

OCENA WARUNKÓW HYDROGEOLOGICZNYCH W MIĘDZYRZECZU KURÓWKI I BYSTREJ (REJON PUŁAW)

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2019-10-07 DOI: 10.7306/bpig.30

R. Zdechlik, P. Pietrzak

{"title":"OCENA WARUNKÓW HYDROGEOLOGICZNYCH W MIĘDZYRZECZU KURÓWKI I BYSTREJ (REJON PUŁAW)","authors":"R. Zdechlik, P. Pietrzak","doi":"10.7306/bpig.30","DOIUrl":"https://doi.org/10.7306/bpig.30","url":null,"abstract":"Badania przeprowadzono w celu oceny warunków hydrogeologicznych pierwszego poziomu wodonośnego w rejonie na wschód od Puław, na obszarze międzyrzecza Kurówki i Bystrej. W ujęciu regionalnym wody podziemne krążą w obrębie pozostających w łączności hydraulicznej pięter wodonośnych: czwartorzędowego, czwartorzędowo-kredowego i kredowego, przy czym dominującą rolę odgrywa piętro kredowe. Rzeki ograniczające obszar mają charakter drenujący i determinują układ pola hydrodynamicznego. Podstawą oceny warunków hydrogeologicznych były własne badania terenowe, obejmujące w 200 studniach pomiary głębokości do zwierciadła wody oraz oznaczenie właściwości fizykochemicznych wód, a z wytypowanych studni dodatkowo pobór próbek do szczegółowych badań laboratoryjnych. Oznaczone w wodach ze wszystkich studni wartości właściwości fizykochemicznych (pH, PEW i temperatury) zasadniczo mieszczą się w zakresie dopuszczalnym dla wód do spożycia. Wyniki szczegółowych oznaczeń laboratoryjnych makro- i mikroskładników w wodach podziemnych wskazują na przewagę słabego stanu chemicznego (6 punktów), w porównaniu do stanu dobrego (2 punkty). W odniesieniu do normatywów dla wód do spożycia, kryteria spełniają wody z 3 punktów, podczas gdy w 5 punktach wymogi nie są spełnione.","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"20 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-10-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133414017","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

TEMPERATURA WÓD PODZIEMNYCH JAKO WSKAŹNIK ZASILANIA NA PRZYKŁADZIE UJĘCIA DLA WROCŁAWIA

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2019-10-07 DOI: 10.7306/BPIG.2

Marek Błachowicz, S. Buczyński, S. Staśko

引用次数: 0

Magmatic episodes in the Holy Cross Mountains, Poland – a new contribution from multi-age zircon populations 波兰圣十字山的岩浆事件——多年龄锆石种群的新贡献

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2019-03-28 DOI: 10.5604/01.3001.0013.0839

E. Krzemińska, L. Krzemiński

引用次数: 2

A FLUORESCENCE CONTRIBUTION TO THE RECOGNITION OF FLUIDS TRAPPED IN MINERALS IN THE CARPATHIAN OUTCROPS 荧光有助于识别喀尔巴阡山脉露头矿物中捕获的流体

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2019-03-28 DOI: 10.5604/01.3001.0013.0825

K. Jarmołowicz-Szulc

{"title":"A FLUORESCENCE CONTRIBUTION TO THE RECOGNITION OF FLUIDS TRAPPED IN MINERALS IN THE CARPATHIAN OUTCROPS","authors":"K. Jarmołowicz-Szulc","doi":"10.5604/01.3001.0013.0825","DOIUrl":"https://doi.org/10.5604/01.3001.0013.0825","url":null,"abstract":"Based on the assumption that fluorescence studies are an important tool in search and characterization of hydrocarbons, samples of rocks, minerals and the organic matter were collected in the Western Carpathian area spreading from the Mszana Górna region in the west to the Bieszczady Mts. in the east, and continuously, towards SE outside the Polish frontier, in Ukraine and Slovakia. Analytical procedures comprised preparation, microscopic observation of the material (organic matter and minerals) from the point of view of inclusions and fluorescence followed by detailed luminescence studies. Those steps have been followed by the microthermometric determinations. The application of the fluid inclusion methods, which are one of the newest analytical tools in the last two decades have led to the characteristics of fluids trapped in the inclusions in the area. The fluorescence studies showed some diversity of hydrocarbons both in compositions and in distribution. The analyses were performed in double-sided polished thin sections prepared based on cold techniques. Fluorescence of inclusions in two minerals, quartz and calcite, was checked in those specific thin sections either in glued wafers, or loose (single) crystals. The fluid inclusion studies were accompanied later on by solid organic matter inclusion studies. Those point to the presence of the following minerals: quartz, dolomite, calcite, clay minerals, gypsum with anhydrite admixture, traces of pyrite and siderite, feldspars. General distribution of fluorescing and not fluorescing inclusions suggests the presence of light hydrocarbons (methane) in the west and south of the area, being enriched in higher hydrocarbons (oil) towards the east.\u0000\u0000","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"25 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-03-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127239490","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

THE CHARACTERISTICS OF PORE SPACE IN LOWER TRIASSIC SANDSTONES OF THE WARSAW REGION 华沙地区下三叠统砂岩孔隙空间特征

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2019-03-28 DOI: 10.5604/01.3001.0013.0826

M. Kuberska, A. Becker, A. Kozłowska

引用次数: 0

Instrumental methods applied in the investigations of carbonate minerals in the Middle Jurassic sideritic rocks with respect to diagenetic processes 应用仪器方法对中侏罗统菱铁矿岩中的碳酸盐矿物进行成岩作用研究

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2019-03-28 DOI: 10.5604/01.3001.0013.0837

A. Kozłowska

{"title":"Instrumental methods applied in the investigations of carbonate minerals in the Middle Jurassic sideritic rocks with respect to diagenetic processes","authors":"A. Kozłowska","doi":"10.5604/01.3001.0013.0837","DOIUrl":"https://doi.org/10.5604/01.3001.0013.0837","url":null,"abstract":"Carbonate minerals in the Middle Jurassic sideritic rocks from the Polish Lowlands, north-eastern margin of the Holy Cross Mountains and the Częstochowa region have been studied applying accessible instrumental methods. The following techniques were applied: polarization microscope, staining with the Evamy’s solution, cathodoluminescence, microprobe, fluid inclusions and isotopic analyses. Most of these methods were not available either in the 20ies of the past century when studies of sideritic iron ores in Poland had begun, or in 50ies and 60ies when they were in full progress. \u0000The sideritic rocks are mainly represented by clayey siderites (they contain also muddy and sandy varieties), sideritic sandstones and sideritic coquina, less frequently by sideritic conglomerates and mudstones. Sideroplesite is the main carbonate mineral that builds the sideritic rocks, while pistomesite and siderite are less frequent. Fe-calcite and Fe-dolomite, ankerite, and sporadic dolomite occur in lesser amounts. \u0000Syderoplesite and siderite have crystallized in the early diagenesis (eodiagenesis), in the zone of microbiologic methanogenesis, at temperatures of about 20°C, from the porous waters of marine origin, or from marine waters mixed with fresh waters. Sideroplesite enriched in magnesium, pistomesite, calcite and ankerite sequently have formed at the later diagenetic stage (mezodiagenesis). These minerals have crystallized at temperatures above 60°C, from the porous waters of marine origin, or from the fluid which interacted with the adjacent rocks. Fe-calcite was formed in the zone of microbiologic methanogenesis, while the ankerite – in the zone of thermal decarboxylation.\u0000\u0000","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"53 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-03-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122268667","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

DETRITAL ZIRCON GEOCHRONOLOGY AND PROVENANCE OF THE PROTEROZOIC QUARTZ-RICH METASEDIMENTS OF THE MAZOWSZE DOMAIN: SOURCE AREAS AND REGIONAL CORRELATION mazowsze域元古代富石英变质沉积岩碎屑锆石年代学与物源:源区与区域对比

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2019-03-28 DOI: 10.5604/01.3001.0013.0840

L. Krzemiński, E. Krzemińska, J. Wiszniewska

引用次数: 1

New achievements in the mineral studies by use of the Raman microspectroscopy 拉曼显微光谱在矿物研究中的新成就

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2019-03-28 DOI: 10.5604/01.3001.0013.0836

K. Jarmołowicz-Szulc, K. Wołkowicz

{"title":"New achievements in the mineral studies by use of the Raman microspectroscopy","authors":"K. Jarmołowicz-Szulc, K. Wołkowicz","doi":"10.5604/01.3001.0013.0836","DOIUrl":"https://doi.org/10.5604/01.3001.0013.0836","url":null,"abstract":"By the means of the technique of the Raman microspectrometry, the complex history of the Earth can be better understood. That is why the Raman spectra determinations are the object of interest in the present paper. The examples of such experiments are presented based on the analyses performed in last years in different scientific centers (Potsdam, Banská Bystrica, Budapest). The identification of inclusion content is shown and the conclusions are drawn for fluid inclusions in some quartz samples from two different localities in Poland – in the Carpathians and in the Fore-Sudetic Block. The implications of the Raman analyses are discussed. It results from the Raman analyses performed that not fluorescing, gas-filled bubbles of huge fluid inclusions from the Jabłonki and Rabe vicinity (the tectonic mélange zone in the Carpathians) have the complex composition of CH4, CO2 and N2 in different mutual proportions dependent on the sample and locality. In another place, despite the fluorescing background, only methane has been identified by Raman spectra. Similar gas composition was determined in the inclusions in the vein quartz in the Wądroże Wielkie area (the Fore-Sudetic Block).\u0000\u0000","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"58 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-03-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"125714165","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

20 YEARS OF EXPERIENCE IN CATHODOLUMINESCENCE RESEARCH AT THE PGI-NRI 在pgi-nri有20年的阴极发光研究经验

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2019-03-28 DOI: 10.5604/01.3001.0013.0841

M. Sikorska-Jaworowska

引用次数: 0

TOTAL POROSITY AND MATRIX PARAMETERS OF CARBONATE ROCKS BASED ON THE ELASTIC WAVE VELOCITY AND DENSITY MEASUREMENTS 基于弹性波速和密度测量的碳酸盐岩总孔隙度和基质参数

Biuletyn Państwowego Instytutu Geologicznego Pub Date : 2018-12-20 DOI: 10.5604/01.3001.0012.7707

J. Jarzyna, E. Puskarczyk, Ewa Ogórek, J. Motyka

引用次数: 0