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Tytuł:
Provenance and tectonic setting of the Middle Eocene lower Akhoreh Formation, Nain area, Central Iran, assessed using petrography and geochemistry
Autorzy:
Salehi, Mohammad Ali
Mallah, Mohammed
Jafarzadeh, Mahdi
Powiązania:
https://bibliotekanauki.pl/articles/27324243.pdf
Data publikacji:
2023
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
petrography
geochemistry
palaeogeography
Nain Ophiolite
Akhoreh Formation
Central Iran
Opis:
The Middle Eocene Akhoreh Formation is superbly exposed in the western corner of the Central-East Iranian Microcontinent (CEIM). This formation covered the northeastern flank of the Cretaceous Nain Ophiolite Mélange (NOM) and is adjacent to the Paleogene Urmieh–Dokhtar Magmatic Arc (UDMA) formed in the southwest of the CEIM. This terrigenous succession is composed of a thin basal conglomerate followed by mostly pink to purple sandstones alternating with shales. The clast composition and clast imbrication of the conglomerates show local source areas towards the north-north-east. Modal components of lower Akhoreh Formation sandstones reveals immature lithic arkose (Q8F48L44) and feldspathic litharenite (Q8F44L48) sandstones that are rich in mafic and ultramafic igneous and volcanic rock fragments. Mafic to ultramafic source rocks are also indicated by geochemical data (enrichment of Mg, Cr and Ni and Cr/V) in the sandstone and shale samples analyzed. However, geochemical data suggests an intermediate igneous rock origin for the shale samples studied, most likely from the nearby continental arc. Based on petrographic data, these sandstones have characteristics of a transitional to undissected arc tectonic setting. Geochemical discrimination diagrams using major and trace elements indicate an oceanic island arc tectonic setting for the lower Akhoreh Formation sandstones and shales, probably due to a predominance of ophiolitic source rocks. Furthermore, the chemical index of alteration and modal analysis indicate a weak to moderate degree of chemical weathering with arid climatic conditions in the source area. The exhumed NOM, together with the UDMA in the southwest, were dominant sources of sediment to the lower Akhoreh Formation, that lay to the northeast in a local retroarc basin of the Central Iranian Microplate, during the Middle Eocene.
Źródło:
Geological Quarterly; 2023, 67, 2; art. no. 14
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Study of Pottery Technology in Kura-Araxes Culture of Astanakroud 2 Site of Kojur County Using Petrographic Method
Autorzy:
Rezaei, Mohammad Hossein
Masjedi Khak, Parastoo
Motavali Rameh, Ali
Powiązania:
https://bibliotekanauki.pl/articles/36182948.pdf
Data publikacji:
2023
Wydawca:
Uniwersytet Przyrodniczo-Humanistyczny w Siedlcach
Tematy:
Archeology
History
Iran
Pottery
Kura-Araxes
Bronze Age
Petrography
Opis:
The pottery samples under investigation in this study include the findings of the Astankroud 2 Site in the Kojur region of western Mazandaran Province. The site was uncovered during an archaeological survey of the region in 2010 and has been thus far the easternmost site of Kura-Araxes. Considering the importance of discussions concerning the characteristics of this culture and the reasons for its spread in a vast geographic area extending from the southern coast of the Caspian Sea to the eastern shores of the Mediterranean Sea, 15 pottery pieces of Kura-Araxes were subject to petrographic study in order to determine the mineralogy structure of the pottery recovered from Astanakroud Site. The experiments on these pieces were conducted using a polarizing microscope (James Swift) at the Petrographic Laboratory of the Institute for Protection and Restoration of Works affiliated with Cultural Heritage Research. According to the results of experiments, it was revealed that all the pottery had been locally produced. A petrographic study of Astanakroud pottery reveals that the pottery has been produced using soil resulting from erosion of geological structure in the northern part of the Kojur region (with volcanic structure) that has been washed up by natural currents traversing the valleys of Nimvar, Avil, and Kouhpar to the foot of the site.
Źródło:
Historia i Świat; 2023, 12
2299-2464
2956-6436
Pojawia się w:
Historia i Świat
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wstępne rozpoznanie petrograficzne i geochemiczne materii organicznej rozproszonej w skałach karbonu Pomorza Zachodniego
Preliminary petrographic and geochemical recognition of organic matter in Carboniferous rocks from Western Pomerania
Autorzy:
Nowak, Grzegorz J.
Karcz, Przemysław
Massalska, Barbara
Powiązania:
https://bibliotekanauki.pl/articles/20241481.pdf
Data publikacji:
2023
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Pomorze Zachodnie
skały carbonu
petrografia organiczna
Piroliza Rock-Evala
skały źródłowe ropy naftowej
Western Pomerania
Carboniferous rocks
organic petrography
Rock-Eval pyrolysis
petroleum source rocks
Opis:
The paper presents results of organic petrography and Rock-Eval pyrolysis studies of Carboniferous rocks from Western Pomerania (N Poland). Samples for the studies were taken from core of the Dźwirzyno 3 borehole. The thermal maturity level of organic matter is determined by the values of: 1) vitrinite reflectance VR o = 0.82-0.93% and 2) T max = 431-460°C, which indicate oil window maturity. Organic petrography studies have shown a presence of different macerals dispersed in the rocks studied. Vitrinite and inertinite are particles of humic origin, while most liptinite macerals are of aquatic provenance. The Rock-Eval data clearly indicate that the organic matter forms levels made up either of kerogen type III or of kerogen type II.
Źródło:
Przegląd Geologiczny; 2023, 71, 4; 224-226
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Petrographic, palynological and geochemical recognition of dispersed organic matter in the black Anthracosia Shales (Sudetes, south-west Poland)
Autorzy:
Nowak, Grzegorz J.
Górecka-Nowak, Anna
Karcz, Przemysław Paweł
Powiązania:
https://bibliotekanauki.pl/articles/2201206.pdf
Data publikacji:
2022
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Intrasudetic Basin
lacustrine black shales
organic petrography
palynofacies
Rock-Eval pyrolysis
petroleum source rocks
Opis:
We describe the organic petrography, palynology and Rock-Eval pyrolysis values of lacustrine black shales termed the Anthracosia Shales (Upper Carboniferous/Lower Permian) in the Intrasudetic Basin (Sudetes, SW Poland). Samples were taken from cores of two boreholes: Rybnica Leśna PIG 1 and Ścinawka Średnia PIG 1. Maceral composition, miospore assemblage composition, palynofacies and geochemical characteristics of dispersed organic matter in the Anthracosia Shales were used to determine conditions of the environment and to evaluate their petroleum potential. Data from both organic petrography and palynology analyses enabled recognition of three broadly distinct organic associations in these shales: bituminous, humic, and intermediate, while Rock-Eval pyrolysis revealed the presence of bituminous and humic kerogen types I and III. Type I corresponds to the bituminous association, with amorphous organic matter (AOM) dominant in the palynofacies, and type III corresponds to the humic association with phytoclasts prevailing in the palynofacies. The thermal maturity of the organic matter is determined by the values of: (1) vitrinite reflectance VRo = 0.53–0.73%, (2) palynomorph 3–4 colour index, and (3) Tmax = 443–447°C, which indicate oil window maturity. Some of the TOC results (1.6–2.9 wt.%) indicate that the Anthracosia Shales are good and very good petroleum source rocks, though the thickness of this interval is low (4–5 m). Shales with TOC values <0.5 wt.% prevail, and may be classifed as poor source rocks.
Źródło:
Geological Quarterly; 2022, 66, 4; art. 66, no. 36
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Source rock potential of the Miocene sedimentary rocks in the Carpathian Foredeep of the Czech Republic
Autorzy:
Geršlová, Eva
Medvecká, Lujza
Jirman, Petr
Nehyba, Slavomír
Opletal, Vladimir
Powiązania:
https://bibliotekanauki.pl/articles/2087030.pdf
Data publikacji:
2022
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Carpathian Foredeep
Miocene
organic petrography
thermal maturity
kerogen type
source rock potential
Opis:
We determine the organic matter content, its thermal maturity, genetic type, and source rock potential of the Miocene sedimentary rocks in the Czech Carpathian Foredeep. In the Czech Republic the Carpathian Foredeep represents a peripheral foreland basin formed due to the tectonic emplacement and loading of the Alpine-Carpathian Thrust Wedge onto the passive margin of the Bohemian Massif. Random vitrinite/huminite reflectance measurements and maceral analyses were performed on 25 samples from the Carpathian Foredeep succession. Additionally, results of 135 TOC content measurements, 141 Rock-Eval pyrolysis analyses and 27 vitrinite reflectance measurements were used to evaluate the regional distribution and depth trends for the entire Carpathian Foredeep. The thermal maturity of organic matter is between the immature part and peak of the oil window (Tmax = 413–448°C). Beneath the Western Carpathian Thrust Belt, the thermal maturity reaches higher values (Rr = 0.43–0.58%, Tmax = 429–448°C). The hydrocarbon generation potential is poor or fair, even if the total organic carbon values indicate good or even very good source rock potential. This is mainly due to the prevailing gas-prone Type III kerogen. The best source rocks were observed in the Miocene strata of the southern and central segments of the area discussed.
Źródło:
Geological Quarterly; 2022, 66, 1; art. no. 1
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Badania mineralogiczno-petrograficzne i chemiczne gnejsu jako klucz do racjonalnej gospodarki złożem
Mineralogical-petrographical and chemical research of gneiss as the key to rational management of mineral deposit
Autorzy:
Kania, Marcin
Zielińska, Amelia
Pomorski, Andrzej
Gunia, Piotr
Majcher, Arkadiusz
Powiązania:
https://bibliotekanauki.pl/articles/2175613.pdf
Data publikacji:
2021
Wydawca:
Poltegor-Instytut Instytut Górnictwa Odkrywkowego
Tematy:
gnejs
metamorfik Doboszowic
petrografia
analizy chemiczne
gospodarka o obiegu zamkniętym
gneiss
Doboszowice metamorphic massif
petrography
chemical analyses
circular economy
Opis:
W artykule scharakteryzowano wyniki analiz petrograficznych i chemicznych gnejsu ze złoża Doboszowice 1. Złoże cechuje się złożoną budową geologiczną, warunkowaną zarówno przez obecność licznych odmian petrograficznych kopaliny, jak i zmienną miąższość nadkładu i występowaniem licznych przerostów i dyslokacji. Analiza budowy złoża ułatwia planowanie selektywnej eksploatacji złoża i dywersyfikację kierunków wykorzystania kopaliny oraz odpadów wydobywczych. Takie działanie wpisuje się w zasady racjonalnej, niskoemisyjnej gospodarki zasobami naturalnymi o obiegu zamkniętym.
Results of the petrographic and chemical analyses of the gneiss from the Doboszowice 1 deposit have been described in this paper. The deposit is characterised by the complicated geological setting, conditioned by the presence of the various petrographic types of gneiss, variable thickness of the cover and the occurence of the mumerous overgrowths and dislocations. The examination of the deposit’s structure makes planning of the selective extraction and diversity of the post-mining wastes usage directions easier. Such activities fit into the rules of rational, low-emission natural resources management and circular economy.
Źródło:
Górnictwo Odkrywkowe; 2021, 62, 3; 4--18
0043-2075
Pojawia się w:
Górnictwo Odkrywkowe
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Coalification as a process determining the methane adsorption ability of coal seams
Autorzy:
Dutka, Barbara
Godyń, Katarzyna
Powiązania:
https://bibliotekanauki.pl/articles/1853877.pdf
Data publikacji:
2021
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
metan
petrografia
adsorpcja
coal bed methane
degree of coalification
petrography
adsorption capacity
Opis:
The paper presents the results of a study of methane adsorption on coal samples with various degrees of metamorphism, coming from the Polish and Czech parts of the Upper Silesian Coal Basin (USCB). The range of coalification of the samples was from bituminous with vitrinite reflectance Ro equal to about 0.5% to para-anthracite coals with Ro equal to over 2%. The methane adsorption capacity was determined at the temperature 303 K for each of the studied coal seams. Methane adsorption isotherms were approximated using the Langmuir model. The relationship between the Langmuir isotherm parameters (am and PL) and the degree of coalification was presented. It was shown that the degree of coalification of the coal substance affects the adsorption ability of coal with respect to methane and determines the value of the Langmuir isotherm parameters. The study was conducted in order to present the distribution of adsorption capacity of Upper Silesian coals in relation to improving work safety in active mines as well as designing technologies that use coal bed methane (CBM) from balance and off-balance resources.
Źródło:
Archives of Mining Sciences; 2021, 66, 2; 181-195
0860-7001
Pojawia się w:
Archives of Mining Sciences
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Petrographic characteristics of the Ordovician and Silurian deposits in the Baltic Basin (N Poland) and their relevance for unconventional hydrocarbon accumulations
Autorzy:
Kuberska, Marta
Sikorska-Jaworowska, Magdalena
Kozłowska, Aleksandra
Podhalańska, Teresa
Powiązania:
https://bibliotekanauki.pl/articles/2060104.pdf
Data publikacji:
2021
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
petrography
mineralogy
shale-type accumulations
total organic carbon
Ordovician rocks
Silurian rocks
Baltic Basin
Opis:
The Ordovician and Silurian deposits in the Baltic Basin are represented by siltstones, mudstones, limestones, marls, sandstones and, most commonly, claystones with a markedly shaley structure. Claystones that are particularly rich in organic matter are considered as potential reservoirs for shale gas accumulations. Samples from 11 boreholes, including core samples of the Piaśnica, Słuchowo, Kopalino, Sasino, Prabuty, Jantar, Pelplin and locally Pasłęk, Kociewie and Puck formations, were analysed by optical microscopy, cathodoluminescence (CL), scanning electron microscopy (SEM) and energy-dispersive spectrometry and X-ray diffraction analyses (XRD). The Piaśnica, Sasino, Jantar, Pasłęk and Pelplin formations are characterized locally by a dominance of black bituminous claystones with a high content of organic matter, and a generally consistent clay mineral composition. Individual samples only show variations in silt fraction and carbonate content. Very important is the negligible proportion of swelling minerals in the clay fraction; the percentage of smectite in the mixed-layered illite/smectite minerals does not exceed 15%. It is important for the rocks to have adequate [SiO2 >10%; Quartz (Q) + Feldspars (Fs) + Carbonates >40%] brittleness. The content of quartz, feldspars and carbonates (here >40%) suggests that the claystones are susceptible to hydraulic fracturing. The claystones show micropores between detrital grains, between the flakes of clay minerals, within pyrite framboids, and organic matter and secondary micropores within grains.
Źródło:
Geological Quarterly; 2021, 65, 3; 65: 44
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Skały osadowe czerwonego spągowca w wierceniu Kutno 2 w warunkach postulowanego jurajskiego wydarzenia termicznego oraz wysokich nadciśnień : studium petrograficzne
Rotliegend sedimentary rocks in the Kutno 2 well under conditions of a postulated Jurassic thermal event and high overpressure : a petrographic study
Autorzy:
Kuberska, Marta
Kiersnowski, Hubert
Poprawa, Paweł
Kozłowska, Aleksandra
Powiązania:
https://bibliotekanauki.pl/articles/2076191.pdf
Data publikacji:
2021
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
basen spągowca polskiego
struktura Kutna
petrografia
termika
Polish Rotliegend Basin
Kutno structure
petrography
thermal history
Opis:
A highs ignifance of the Kutno 2 deep borehole is due to its location in the central zone of the Polish Basin where the Rotliegend complex has previously never been achieved by other drill holes and thus was not recognized and studied. Drill core from the Rotligend of the Kutno2 has been recently studied for its petrography and facies. The Rotligend in this zone is represented by fluvial and alluvial sediments. It is composed mainly of fine- to coarse-grained sandstones, with conglomerate inter beds. Diagenetic processes of the sediments have been dominated by mechanical and chemical compaction, as well as by transformation of the unstable mineral components. Fluid inclusion analysis for quartz and carbonates indicates that the diagenesis-associated temperature reached 120-180°C. The presence of haematite pseudomorphoses after framboidal pyrite indicates an extremely high palaeotemperature of approx. 500°C. Itis related here to the Jurassic hydrothermal event. The recent very high reservoir pressure might be associated with high temperatures due to the aqua thermal pressure mechanism.
Źródło:
Przegląd Geologiczny; 2021, 69, 6; 365--373
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
A putative Tournaisian and Visean volcanic-sedimentary succession in the Lublin Basin, SE Poland: depositional processes, petrological characteristics and sequence stratigraphy
Autorzy:
Waksmundzka, Maria I.
Kozłowska, Aleksandra
Pańczyk, Magdalena
Powiązania:
https://bibliotekanauki.pl/articles/1835593.pdf
Data publikacji:
2020
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Tournaisian
Visean
Lublin basin
sequence stratigraphy
petrography
cyclothems
volcanic source areas
turnej
wizen
niecka lubelska
stratygrafia sekwencji
petrografia
cyklotemy
Opis:
The aim of this study was to establish the stratigraphic extent of a putative Tournaisian Stage within the Carboniferous succession in the Lublin Basin. The oldest part of the succession, known as the Huczwa Formation and comprising depositional sequences 1-4, was investigated based on lithofacies analysis, sequence stratigraphy and petrographic studies. The article provides descriptions of depositional sequences, parasequences (cyclothems) and lithofacies that were formed in a range of environments (elements of depositional architecture) and as a result of volcanic processes - lava and pyroclastic eruptions and chemical weathering of their products. Correlation of the sequence stratigraphy to the West European and global Carboniferous chronostratigraphic divisions, as well as to the Khoriv suite in the Lviv-Volyn Basin in adjacent Ukraine, indicates a putative late Tournaisian age for sequence 1, and a late Visean age for sequences 2-4. There is a stratigraphic gap between sequences 1 and 2, spanning probably the uppermost Tournaisian and the lower and middle Visean. The upper Tournaisian is represented by the FRST-LST deposits of sequence 1, comprising mainly volcaniclastic conglomerates and sandstones developed in braided-river channels and incised valleys with hyperconcentrated flow processes. These deposits are represented by polymictic paraconglomerate and lithic/sublithic/subarkose arenites or sublithic wackes, and contain predominantly grains of acidic and alkaline volcanic and igneous rocks. This material probably came from the Łuków-Wisznice Elevation and the Volynian Polesia region, located to the NE and E of the Lublin Basin. In the uppermost part of sequence 1, volcanic rocks and tuffs appear which developed during the activity of at least three volcanic cones in the Lublin Basin. The volcanoes were the source of alkaline lavas in the central and SW areas of the basin, and of acidic lavas in the SE area, previously undescribed. The Visean sequences 2-4 consist of the FRST-LST sediments deposited within incised valleys. The TST and HST deposits accumulated mainly in a shallow ramp-type carbonate shelf, shallow clayey shelf and deltaic environments.
Źródło:
Acta Geologica Polonica; 2021, 71, 3; 305-344
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Charakterystyka utworów czerwonego spągowca w aspekcie badań rentgenowskiej mikrotomografii komputerowej i mikroskopii optyczne
Characteristics of Rotliegend sediments in view of X-ray microtomohraphy and optical microscopy investigations
Autorzy:
Dohnalik, Marek
Ziemianin, Konrad
Powiązania:
https://bibliotekanauki.pl/articles/1833915.pdf
Data publikacji:
2020
Wydawca:
Instytut Nafty i Gazu - Państwowy Instytut Badawczy
Tematy:
czerwony spągowiec
mikrotomografia
petrografia
własności zbiornikowe
Rotliegend
microtomography
petrography
reservoir properties
Opis:
The article presents the results of microtomographic and petrographic investigations of Rotliegend sandstones collected from core material from wells located in the area of the Fore-Sudetic Monocline in its central and northern parts and also on the border of the Fore-Sudetic Monocline and the Mogilno - Łódź Synclinorium. Three areas were selected for the study: Czarna Wieś–Parzęczewo (19 samples), Środa Wielkopolska–Kromolice (21 samples) and Siekierki–Miłosław (21 samples). The aim of the petrologic and microtomographic studies was to investigate how the different reservoir properties of sandstones will be reflected in the results of the methods used. Strong differences between samples from the region of Środa Wielkopolska–Kromolice and the other studied areas have been demonstrated. In the case of this area several key factors were noticed: the highest average value of effective porosity; the highest average content of pores belonging to class VII (pore volume subsystem classification); three times higher average value of the CT porosity coefficient and the largest length of the average chord. Also in terms of petrography (composition of grains, cement type) it is a region where major differences, especially compared to the region of Czarna Wieś–Parzęczewo, can be seen. Based on the obtained results, it was possible to rank the examined regions in terms of their reservoir properties – from the worst (Czarna Wieś–Parzęczewo) to the best (Środa Wielkopolska–Kromolice). These conclusions are also confirmed by other petrophysical analyses (eg. mercury porosimetry, permeability analysis). Combination of the obtained microtomographic and petrographic results allowed to obtain a full characterization of the investigated samples – both in terms of the mineralogical composition of grains, as well as the development of the pore space. These data, especially in combination with the results of density and porosity analyses (helium pycnometry and mercury porosimetry), open up a number of possibilities to carry out different types of modeling (porosity, permeability) both on the scale of the sample itself, as well as the scale of a single well or even the whole basin, which is crucial for creating a hydrocarbon exploration strategy.
Źródło:
Nafta-Gaz; 2020, 76, 11; 765--773
0867-8871
Pojawia się w:
Nafta-Gaz
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Comparative petrography and organic geochemistry of different types of organic matter occurring in the Outer Carpathians rocks
Autorzy:
Zielińska, Magdalena
Fabiańska, Monika
Więcław, Dariusz
Misz-Kennan, Magdalena
Powiązania:
https://bibliotekanauki.pl/articles/2058565.pdf
Data publikacji:
2020
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Polish Outer Carpathians
redeposited organic matter
organic matter petrography
thermal maturity
biomarkers
Rock-Eval
Opis:
The characterization of organic matter (OM) in sedimentary rocks is important in many types of biological, geological and environmental research. The integrated use of microscopy and geochemistry, as here, is particularly useful in any attempt to define the origin and evolution of OM in sedimentary basins. The organic petrography and geochemistry different types of allogenic and authigenic OM from the Polish Outer Carpathian (POC) rocks were studied in present study to compare their genetic type, thermal maturity, depositional environment and post-sedimentation processes. Special attention was paid to redeposited coal clasts occurrences. The used techniques show differences in organic matter type originating from various sources. The organic petrography analysis shows that redeposited coal clasts (CC) and terrigenous organic matter (TOM) are composed predominantly of woody material (the gas-prone Type-III kerogen). Similar results were obtained during the Rock-Eval pyrolysis. Moreover, the GC-MS analysis of extracts indicated the additional source of OM, namely planktonic organic matter (POM) with oil-prone kerogen Type-I or II. This OM is in some cases high thermally mature and could potentially has allochthonous origin. The n-alkane, saturated and aromatic biomarker data revealed deposition of this POM in anoxic deltaic or close-shore sedimentary environments whereas the redeposited coal clasts were probably originally deposited in coal swamps as were the Upper Silesian bituminous coals.
Źródło:
Geological Quarterly; 2020, 64, 1; 165--184
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Mineralogical study and enhanced gravity separation of gold-bearing mineral, South Eastern Desert, Egypt
Autorzy:
El-Sayed, Samah
Abdel-Khalek, N. A.
El-Shatoury, E. H.
Abdel-Motelib, A.
Hassan, M. S.
Abdel-Khalek, M.A.
Powiązania:
https://bibliotekanauki.pl/articles/1845207.pdf
Data publikacji:
2020
Wydawca:
Politechnika Wrocławska. Oficyna Wydawnicza Politechniki Wrocławskiej
Tematy:
gold
mineralogy
petrography
gravity separation
Falcon concentrator
Opis:
El-Hudi gold deposit, located in the South Eastern Desert of Egypt, represent large vein- type gold occurrence. The representative sample revealed the abundance of quartz as main constituent with minor amounts of mineral impurities. Gold was detectable (12 g/t) as determined using atomic absorption. The petrographic study revealed that the gold grains ranged from 10-40 μm. The grain boundaries of quartz are highly stained with iron minerals as hematite and limonite. Sericite mineral is common in discrete gold-bearing veins. Eroded pyrite was detected with high alteration leaving only cubic-shaped cavities behind. Different techniques for gravity separation were used to separate gold from the quartz mineral. After crushing and grinding of the sample, shaking table was used to upgrade the coarser fractions while Falcon concentrator was employed to upgrade the fine fraction. The best concentrate was obtained through grinding the whole sample to less than 0.2 mm, followed by cleaning steps. The gold content is increased from 12 to 145 g/t with total recovery of 78%.
Źródło:
Physicochemical Problems of Mineral Processing; 2020, 56, 5; 839-848
1643-1049
2084-4735
Pojawia się w:
Physicochemical Problems of Mineral Processing
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Pigment mineralogy, chemical composition and stratigraphy of wall paintings in the Church in Włościejewki, Poland
Mineralogia pigmentów, skład chemiczny i stratygrafia malowideł ściennych w kościele we Włościejewkach w Polsce
Autorzy:
Węcławska, Marta
Powiązania:
https://bibliotekanauki.pl/articles/1841687.pdf
Data publikacji:
2020
Wydawca:
Stowarzyszenie Konserwatorów Zabytków
Tematy:
pigments
thin section
wall paintings
microstratigraphy
petrography
pigmenty
cienkie płytki
malowidła ścienne
mikrostratygrafia
petrografia
Opis:
The sixteenth-century geometrical polychromies that were discovered during conservation works in a medieval church in Włościejewki provided an extraordinary opportunity to examine the original structure of old painting layers and compare them with newer ones. Scientific research was carried out to obtain and confirm the stratigraphy of the paintings and enhance the knowledge about the techniques and pigments that had been used there. This paper presents a mineralogical and petrographic characteristic of the materials. The analysis was performed in painting layers such as: plaster, whitewash and pigment. They originated from layers created between the sixteenth and nineteenth century. Four microscopic observations of thin sections were made, using reflected and transmitted light. Samples that turned out to be too fragile were examined using a scanning microscope equipped with an EDS detector. The research also described in detail the plaster and the whitewash. Monochromes of the background, details of walls and ceilings were made on lime whitewash using the dry fresco technique. The study illustratively demonstrates the structural and textural variability of the painting layers through the ages. The study’s findings show a slight variability of the pigments, mainly iron oxides based pigments.
Szesnastowieczne polichromie geometryczne, które odkryto podczas prac konserwatorskich w średniowiecznym kościele we Włościejewkach, dostarczyły nadzwyczajnej możliwości zbadania oryginalnej struktury starych warstw malarskich i porównania ich z nowszymi warstwami. Przeprowadzono badania naukowe, aby otrzymać i potwierdzić stratygrafię malowideł i pogłębić wiedzę na temat użytych technik i pigmentów. Niniejszy artykuł prezentuje mineralogiczną i petrograficzną charakterystykę zastosowanych materiałów. Analizę przeprowadzono na takich warstwach malarskich, jak: tynki, farba wapienna i pigmenty. Zostały one pobrane z warstw wytworzonych pomiędzy XVI i XIX wiekiem. Wykonano cztery obserwacje mikroskopowe na preparatach, wykorzystując światło odbite i przechodzące. Próbki, które okazały się zbyt delikatne, zostały przebadane przy użyciu mikroskopu skanującego wyposażonego w detektor EDS. Badanie również szczegółowo opisało tynk i farbę wapienną. Monochromie tła, detale ścian oraz sufitów wykonano na farbie wapiennej przy użyciu techniki suchego fresku. Badanie ilustratywnie przedstawia strukturalne i teksturalne zróżnicowanie warstw malarskich w różnych wiekach. Wyniki pokazują nieznaczne zróżnicowanie w pigmentach, głównie opartych na tlenkach żelaza.
Źródło:
Wiadomości Konserwatorskie; 2020, 64; 161-171
0860-2395
2544-8870
Pojawia się w:
Wiadomości Konserwatorskie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wyniki badań petrograficzno-mineralogicznych wybranych kamieni młyńskich z terenu Pomorza. Przyczynek do zastosowania interdyscyplinarnych metod w badaniach nad tradycyjnym młynarstwem
Results of petrographic and mineralogical research of selected millstones from Pomerania – a contribution to the use of interdisciplinary methods in research on traditional milling
Autorzy:
Bartz, Wojciech
Prarat, Maciej
Powiązania:
https://bibliotekanauki.pl/articles/217486.pdf
Data publikacji:
2020
Wydawca:
Stowarzyszenie Konserwatorów Zabytków
Tematy:
petrografia
młyny wodne
wiatraki
kamienie młyńskie
petrography
watermills
windmills
millstones
Opis:
Kamienie młyńskie od wieków były głównym elementem systemu roboczego zakładów napędzanych siłą wody i wiatru. Te niezwykle cenne zabytki kultury materialnej rozpoznane są jednak w nieznacznym zakresie. W ostatnich latach widoczna jest intensyfikacja interdyscyplinarnych metod badawczych w molinologii. Jedną z nich są badania petrograficzne kamieni młyńskich. W polskich opracowaniach brak jednak takiego ujęcia. Dla wybranej, skatalogowanej grupy kamieni z terenów Pomorza autorzy obrali za cel określenie rodzaju skał, miejsca ich pochodzenia oraz funkcji w młynie. Spośród 15 kamieni trzy okazały się sztucznym kamieniem, 8 piaskowcem kwarcowym, jedna granitem, jedna anortozytem kwarcowym, dwie skałą osadową krzemionkową. Dla części udało się także określić miejsce pochodzenia z łomów niemieckich i francuskich, niektóre mogły być pochodzenia miejscowego.
Millstones have been the main element of the working system of plants powered by water and wind for centuries. However, these extremely valuable monuments of material culture are recognized to a rather small extent. Recent years have seen a certain intensification of interdisciplinary research in the field of molinology. One of them is petrographic study of millstones. Yet, Polish studies still lack this kind of approach. This paper is aimed at determining the types of rocks, their origins and functions within the mill structure. In a group of fifteen stones, three were made of artificial stone, eight turned out to be quartz sandstones, one is made of granite and one of quartz anorthosite, two proved to be made of sedimentary siliceous rock. Certain rocks have been determined to be of German or French origin, whereas the others could have been acquired locally.
Źródło:
Wiadomości Konserwatorskie; 2020, 61; 124-144
0860-2395
2544-8870
Pojawia się w:
Wiadomości Konserwatorskie
Dostawca treści:
Biblioteka Nauki
Artykuł
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