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.
{"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}
Celem badań jest testowanie metody i wstępna ocena wielkości infiltracji efektywnej na podstawie wyników pomiarów temperatury w piezometrach w otoczeniu studni i stawów infiltracyjnych na terenach wodonośnych Wrocławia. Badania zmienności temperatury wód podziemnych w sieci obserwacyjnej na obszarze sztucznej infiltracji przeprowadzono w sieci 11 piezometrów. Wody pierwszego poziomu wodonośnego występują w aluwialnych osadach piaszczystych i zalegają na głębokościach 2–12 m. Roczne pomiary temperatur wód podziemnych w sieci obserwacyjnej na stałej głębokości (3–4 m) wykazały szeroki zakres zmian od 1,5 do 25,9°C. Przedstawiono charakterystyczne i typowe zakresy średnich zmian temperatur w przedziale 9,3–15,6°C zarejestrowane w 2018 r. Na podstawie profilowania termicznego w wybranym punkcie obliczono średnią wartość zasilania, stosując metodykę zaproponowana przez Taniguchiego (1993, 1994). Obliczona wstępnie wartość sztucznego zasilania wynosi 20,19 mm/d i odpowiada wielkości zasobów obliczonych na podstawie modelowania numerycznego.
{"title":"TEMPERATURA WÓD PODZIEMNYCH JAKO WSKAŹNIK ZASILANIA NA PRZYKŁADZIE UJĘCIA DLA WROCŁAWIA","authors":"Marek Błachowicz, S. Buczyński, S. Staśko","doi":"10.7306/BPIG.2","DOIUrl":"https://doi.org/10.7306/BPIG.2","url":null,"abstract":"Celem badań jest testowanie metody i wstępna ocena wielkości infiltracji efektywnej na podstawie wyników pomiarów temperatury w piezometrach w otoczeniu studni i stawów infiltracyjnych na terenach wodonośnych Wrocławia. Badania zmienności temperatury wód podziemnych w sieci obserwacyjnej na obszarze sztucznej infiltracji przeprowadzono w sieci 11 piezometrów. Wody pierwszego poziomu wodonośnego występują w aluwialnych osadach piaszczystych i zalegają na głębokościach 2–12 m. Roczne pomiary temperatur wód podziemnych w sieci obserwacyjnej na stałej głębokości (3–4 m) wykazały szeroki zakres zmian od 1,5 do 25,9°C. Przedstawiono charakterystyczne i typowe zakresy średnich zmian temperatur w przedziale 9,3–15,6°C zarejestrowane w 2018 r. Na podstawie profilowania termicznego w wybranym punkcie obliczono średnią wartość zasilania, stosując metodykę zaproponowana przez Taniguchiego (1993, 1994). Obliczona wstępnie wartość sztucznego zasilania wynosi 20,19 mm/d i odpowiada wielkości zasobów obliczonych na podstawie modelowania numerycznego.","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"61 2 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":"133672502","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}
Pub Date : 2019-03-28DOI: 10.5604/01.3001.0013.0839
E. Krzemińska, L. Krzemiński
This contribution reports on new U–Pb zircon age data from magmatic rocks from the Holy Cross Mountains (HCM) of Poland. The analyzed samples were taken from lamprophyre and diabase veins of Podkranów and Janowice-2 as well as from tuff horizon of Kielce Beds (Ludlow). Internal morphologies have been investigated by SEM-BSE and cathodoluminescence images and they have been used as a guide for the selection of genetically various type of grains, e.g. potential auto-, ante- and xenocrysts, that were analyzed by ion microprobe. The U–Pb age of the magmatic events at 414.2 ±6.6 Ma (Kielce tuff), 322 ±12 Ma (Podkranów, lamprophyre), and 300±10 Ma (Janowice-2, diabase) confirmed the time frame of known magmatic activity reported within the HCM, as determined by 40Ar/39Ar geochronology in previous studies. The zircon investigation revealed also multiple populations with record of an earlier pulse of magma system (antecrysts), as well as abundant xenocrysts.
本文报道了波兰圣十字山(HCM)岩浆岩中新的U-Pb锆石年龄数据。分析样品取自Podkranów和Janowice-2的煌斑岩和辉绿岩脉，以及Kielce床(Ludlow)的凝灰岩层。利用SEM-BSE和阴极发光图像研究了其内部形态，并用离子探针分析了潜在的自晶、前晶和异晶等不同基因类型的晶粒的选择。岩浆活动的U-Pb年龄分别为414.2±6.6 Ma (Kielce凝灰岩)、322±12 Ma (Podkranów煌斑岩)和300±10 Ma (Janowice-2辉绿岩)，证实了HCM内已知岩浆活动的时间框架，即先前研究中40Ar/39Ar的地质年代学。锆石研究还发现了多个具有早期岩浆系统脉冲记录的种群(前结晶)，以及丰富的异结晶。
{"title":"Magmatic episodes in the Holy Cross Mountains, Poland – a new contribution from multi-age zircon populations","authors":"E. Krzemińska, L. Krzemiński","doi":"10.5604/01.3001.0013.0839","DOIUrl":"https://doi.org/10.5604/01.3001.0013.0839","url":null,"abstract":"This contribution reports on new U–Pb zircon age data from magmatic rocks from the Holy Cross Mountains (HCM) of Poland. The analyzed samples were taken from lamprophyre and diabase veins of Podkranów and Janowice-2 as well as from tuff horizon of Kielce Beds (Ludlow). Internal morphologies have been investigated by SEM-BSE and cathodoluminescence images and they have been used as a guide for the selection of genetically various type of grains, e.g. potential auto-, ante- and xenocrysts, that were analyzed by ion microprobe. The U–Pb age of the magmatic events at 414.2 ±6.6 Ma (Kielce tuff), 322 ±12 Ma (Podkranów, lamprophyre), and 300±10 Ma (Janowice-2, diabase) confirmed the time frame of known magmatic activity reported within the HCM, as determined by 40Ar/39Ar geochronology in previous studies. The zircon investigation revealed also multiple populations with record of an earlier pulse of magma system (antecrysts), as well as abundant xenocrysts.\u0000\u0000","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"57 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":"115426197","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}
Pub Date : 2019-03-28DOI: 10.5604/01.3001.0013.0825
K. Jarmołowicz-Szulc
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.
{"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}
Pub Date : 2019-03-28DOI: 10.5604/01.3001.0013.0826
M. Kuberska, A. Becker, A. Kozłowska
Reservoir and sealing properties of Lower Triassic sandstones from seven boreholes of the central part of the Koszalin-Zamość Synclinorium were investigated in terms of potential levels for underground storage of carbon dioxide. Extensive petrographic studies, image analysis, and investigations of petrophysical properties of rocks and pore space were carried out. The research shows that diagenetic processes both variously affected the intensity of alteration and variously shaped the pore space. Not only primary but also secondary porosity, resulting from diagenetic alteration and dissolution, is observed in the rocks. Microscopic observations revealed that the pore space in studied samples is dominated by macropores. The results obtained indicate a poor suitability of the Lower Triassic deposits for the purpose of carbon dioxide sequestration.
{"title":"THE CHARACTERISTICS OF PORE SPACE IN LOWER TRIASSIC SANDSTONES OF THE WARSAW REGION","authors":"M. Kuberska, A. Becker, A. Kozłowska","doi":"10.5604/01.3001.0013.0826","DOIUrl":"https://doi.org/10.5604/01.3001.0013.0826","url":null,"abstract":"Reservoir and sealing properties of Lower Triassic sandstones from seven boreholes of the central part of the Koszalin-Zamość Synclinorium were investigated in terms of potential levels for underground storage of carbon dioxide. Extensive petrographic studies, image analysis, and investigations of petrophysical properties of rocks and pore space were carried out. The research shows that diagenetic processes both variously affected the intensity of alteration and variously shaped the pore space. Not only primary but also secondary porosity, resulting from diagenetic alteration and dissolution, is observed in the rocks. Microscopic observations revealed that the pore space in studied samples is dominated by macropores. The results obtained indicate a poor suitability of the Lower Triassic deposits for the purpose of carbon dioxide sequestration.","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"24 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":"134174159","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}
Pub Date : 2019-03-28DOI: 10.5604/01.3001.0013.0837
A. Kozłowska
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. The 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. Syderoplesite 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.
{"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}
Pub Date : 2019-03-28DOI: 10.5604/01.3001.0013.0840
L. Krzemiński, E. Krzemińska, J. Wiszniewska
Drilling at Mońki IG-2 and Zabiele IG-1 in the Mazowsze domain has intersected mature quartz-rich metasedimentary rocks belonging to the basement of NE Poland, described so far as a Biebrza complex. The geochemical composition of these rocks is characteristic of a passive margin. The subarkose–quartz arenite underwent low-T metamorphism, but preserved textures typical for the fluvial sediments. The detrital material in range 1.68–2.11 Ga was provided from surrounding late Paleoproterozoic margins of the Fennoscandia and Sarmatia. The maximum depositional age probably did not exceed 1.6 Ga. A previously suggested correlation with Mesoproterozoic molasse-type deposits of the Jotnian formation has not been confirmed. It seems more likely that the sediments formed after Fennoscandia-Sarmatia collision (i.e. termination of Svecofennian orogeny) but before denudation of the Mesoproterozoic Mazury AMCG intrusions.
{"title":"DETRITAL ZIRCON GEOCHRONOLOGY AND PROVENANCE OF THE PROTEROZOIC QUARTZ-RICH METASEDIMENTS OF THE MAZOWSZE DOMAIN: SOURCE AREAS AND REGIONAL CORRELATION","authors":"L. Krzemiński, E. Krzemińska, J. Wiszniewska","doi":"10.5604/01.3001.0013.0840","DOIUrl":"https://doi.org/10.5604/01.3001.0013.0840","url":null,"abstract":"Drilling at Mońki IG-2 and Zabiele IG-1 in the Mazowsze domain has intersected mature quartz-rich metasedimentary rocks belonging to the basement of NE Poland, described so far as a Biebrza complex. The geochemical composition of these rocks is characteristic of a passive margin. The subarkose–quartz arenite underwent low-T metamorphism, but preserved textures typical for the fluvial sediments. The detrital material in range 1.68–2.11 Ga was provided from surrounding late Paleoproterozoic margins of the Fennoscandia and Sarmatia. The maximum depositional age probably did not exceed 1.6 Ga. A previously suggested correlation with Mesoproterozoic molasse-type deposits of the Jotnian formation has not been confirmed. It seems more likely that the sediments formed after Fennoscandia-Sarmatia collision (i.e. termination of Svecofennian orogeny) but before denudation of the Mesoproterozoic Mazury AMCG intrusions.\u0000\u0000","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"5 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":"128642789","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}
Pub Date : 2019-03-28DOI: 10.5604/01.3001.0013.0836
K. Jarmołowicz-Szulc, K. Wołkowicz
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).
{"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}
Pub Date : 2019-03-28DOI: 10.5604/01.3001.0013.0841
M. Sikorska-Jaworowska
The use of catholuminescence analysis in scientific research at the PGI-NRI has a 20-year history. The method, combined with other analytical techniques, has become an effective tool in widely understood mineralogical and petrographic investigation reported in numerous publications.
{"title":"20 YEARS OF EXPERIENCE IN CATHODOLUMINESCENCE RESEARCH AT THE PGI-NRI","authors":"M. Sikorska-Jaworowska","doi":"10.5604/01.3001.0013.0841","DOIUrl":"https://doi.org/10.5604/01.3001.0013.0841","url":null,"abstract":"The use of catholuminescence analysis in scientific research at the PGI-NRI has a 20-year history. The method, combined with other analytical techniques, has become an effective tool in widely understood mineralogical and petrographic investigation reported in numerous publications.\u0000\u0000","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"47 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":"124847747","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}
Pub Date : 2018-12-20DOI: 10.5604/01.3001.0012.7707
J. Jarzyna, E. Puskarczyk, Ewa Ogórek, J. Motyka
The purpose of the research was to find relationship between elastic waves velocities obtained from lab measurements and parameters from hydrogeological research. Measurements were conducted on 73 rock samples originating mostly from Jurassic limestone of the Olkusz area. Additional information about the rock samples was obtained when the elastic wave velocities were compared with reservoir parameters such as porosity, permeability and density. Plots of elastic waves velocities vs. porosity and bulk density vs. porosity gave information about the range of P wave velocities from the boundary velocity to the values when porosity is equal to zero. Matrix velocity and density values were introduced into the formulas used to calculate porosity. Anisotropy analysis was made on the basis of elastic wave velocities measured on cores cut in two perpendicular directions. This allowed for identification of fractures in rocks. Results showed that by comparing various petrophysical parameters it was possible to get better information about reservoir properties of aquifers.
{"title":"TOTAL POROSITY AND MATRIX PARAMETERS OF CARBONATE ROCKS BASED ON THE ELASTIC WAVE VELOCITY AND DENSITY MEASUREMENTS","authors":"J. Jarzyna, E. Puskarczyk, Ewa Ogórek, J. Motyka","doi":"10.5604/01.3001.0012.7707","DOIUrl":"https://doi.org/10.5604/01.3001.0012.7707","url":null,"abstract":"The purpose of the research was to find relationship between elastic waves velocities obtained from lab measurements and parameters from hydrogeological research. Measurements were conducted on 73 rock samples originating mostly from Jurassic limestone of the Olkusz area. Additional information about the rock samples was obtained when the elastic wave velocities were compared with reservoir parameters such as porosity, permeability and density. Plots of elastic waves velocities vs. porosity and bulk density vs. porosity gave information about the range of P wave velocities from the boundary velocity to the values when porosity is equal to zero. Matrix velocity and density values were introduced into the formulas used to calculate porosity. Anisotropy analysis was made on the basis of elastic wave velocities measured on cores cut in two perpendicular directions. This allowed for identification of fractures in rocks. Results showed that by comparing various petrophysical parameters it was possible to get better information about reservoir properties of aquifers.\u0000\u0000","PeriodicalId":321173,"journal":{"name":"Biuletyn Państwowego Instytutu Geologicznego","volume":"163 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":"122216890","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}
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