Stability relations of monazite-(Ce), gadolinite-(Ce), gadolinite-(Y), britholite-(Ce) and bastnäsite-(Ce) during late- to post-magmatic processes in nepheline syenite (Čistá pluton, Czech Republic)

Author(s):  
Maciej Jaranowski ◽  
Bartosz Budzyń ◽  
Gabriela A. Kozub-Budzyń ◽  
Jiří Sláma ◽  
Josef Klomínský

<p>Stability relations of the REE-bearing accessory phases and alteration processes in the cancrinite-bearing nepheline syenite from the Čistá pluton (the center of the upper-crustal Tepla–Barrandian unit, Bohemian Massif, Czech Republic) were studied. Observations of rock microtextures, quantitative analyses of minerals and compositional X-ray mapping were performed using electron probe microanalysis (EPMA). The primary REE-bearing accessory minerals assemblage includes monazite-(Ce) associated with gadolinite-group minerals (i.e. gadolinite-(Ce) and gadolinite-(Y)), which were partially replaced by britholite-(Ce), bastnäsite-(Ce), aggregates of fine-grained REE-bearing phases (possibly fluorapatite and/or britholite-(Ce)) and, rarely, cerianite. K-feldspar and albite form intergrowths or symplectites with REE-phases in the investigated reaction microtextures. Furthermore, the zircon crystals demonstrate oscillatory zoning and/or extensive patchy zoning due to alteration processes. The alteration of accessory minerals are interpreted as driven by K- and Na-bearing alkali fluids with high CO<sub>2</sub> activity during late- to post-magmatic processes.</p><p>Acknowledgements: This work was supported by the National Science Centre research grant no. 2017/27/B/ST10/00813.</p>

Author(s):  
Jordan A. Roberts ◽  
Lee A. Groat ◽  
Paul G. Spry ◽  
Jan Cempírek

ABSTRACT The Deer Horn deposit, located 150 km south of Smithers in west-central British Columbia, is an Eocene polymetallic system enriched in Au-Ag-Te with lesser amounts of Bi-Pb-W; the Au and Ag are hosted in Te-bearing minerals and Ag-rich gold (Au-Ag alloy). A quartz-sulfide vein system containing the main zones of Au-Ag-Te mineralization and attendant sericite alteration occurs in the hanging wall of a local, spatially related thrust fault and is genetically related to the nearby Eocene Nanika granodiorite intrusive suite. Tellurium-bearing minerals commonly form isolated euhedral to subhedral grains or composite grains (up to 525 μm in size) of Ag-, Bi-, Pb-, and Au-rich tellurium-bearing minerals (e.g., hessite, tellurobismuthite, volynskite, altaite, and petzite). Panchromatic cathodoluminescence imaging revealed four generations of quartz. Within remnant cores of quartz I, local oscillatory zoning occurs in quartz II. Fine-grained veinlets of quartz III and IV crosscut quartz I and II, showing evidence of at least two deformation events; late-forming veinlets of calcite crosscut all generations of quartz. The tellurides and Ag-rich gold occur in stage III quartz. Three types of fluid inclusions were observed in stage III and IV quartz: (1) aqueous liquid and vapor inclusions (L-V); (2) aqueous carbonic inclusions (L-L-V); and (3) carbonic inclusions (vapor-rich). Primary fluid inclusions related to the telluride mineralization within quartz III were tested with microthermometry, along with a few primary inclusions from quartz IV. Homogenization temperatures are 130.0–240.5 °C for L-V inclusions and 268.0–336.4 °C for L-L-V inclusions. Aqueous carbonic inclusions had solid CO2 melting temperatures from –62.1 to –56.8 °C, indicating the presence of ≈1 to 30 mol.% dissolved methane in these inclusions. The Deer Horn Au-Ag-Te-(Bi-Pb-W) deposit is a reduced intrusion-related gold system characterized by sheeted veins, metal zoning, low salinity aqueous-carbonic fluids, and a genetic relationship to an Eocene granodiorite. Values of δ34S of pyrite vary from –1.6 to 1.6 per mil and are compatible with a magmatic source of sulfur.


2020 ◽  
Vol 41 ◽  
pp. 54-67
Author(s):  
N.М. Lyzhachenkо ◽  
◽  
S.I. Kurylo ◽  
S. M. Bondarenko ◽  
◽  
...  

The Stankuvatske Li deposit (SD) is situated at western flank of the Lypniazka structure (Ingul megablock of the Ukrainian Shield). Knowledge about REE content in host metamorphic rocks is based on the results of bulk chemical analysis, but their minerals have not been determined. For the first time rare-earth mineralization of the Stankuvatsky lithium deposit has been investigated in fine-grained gneiss with «augen» and schistose structure, porphiroblastic texture, formed as result of tectonical alteration. Our investigations were carried out using petrographic and microprobe analysis (EPMA). Mineralogically gneisses consist of quartz, plagioclase, zoizite, biotite, graphite, chlorite and abundant sulphides mainly represented by pyrite, arsenopyrite, sphalerite, molibdenite. Accessory minerals presented by titanite, apatite, monazite, zircon and coffinite. Gneisses have been subjected to deformation and hydrothermal — metasomatic alteration. An investigation of rock-forming and accessory minerals allows to revel low-temperature alterations of primary allanite by bastnäsiteand chlorite with formation of secondary bastnäsite-chlorite-coisite-pyrite association with «coronary» texture. The penetration of S, F, CO2, H2O enriched fluids were caused disintegration, partial redistribution and reprecipitation of rare earth elements. As result synhysite-chlorite-pyrite association was formed.


2016 ◽  
Vol 45 (1) ◽  
pp. 175-186
Author(s):  
Joanna Grzybek

Abstract The paper deals with terminological issues in legal translation. The author has researched the process of establishing equivalents for partially equivalent terminology, using the parametrical approach to legal translation. The research consists of the terminological analysis of the texts of mediation regulations formulated in Chinese and Polish. The objective was to establish translational equivalents in the case of significant differences between the legal systems of the above mentioned linguistic area. The research was financed from the research grant no. 2012/07/E/HS2/00678, titled: Parameterisation of legilinguistic translatology in the scope of civil law and civil procedure awarded by the National Science Centre of the Republic of Poland (Sonata Bis program). Determining the acceptability of functional equivalents in the selected linguistic area is possible by comparison of their semantics with the legal structure in different legal systems and cultures. The author investigates if attributing properties from dimensions relevant in translation to mediation law terms can be helpful in the process of translation.


2021 ◽  
Vol 77 (1) ◽  
pp. 17-35
Author(s):  
Pavel Bokr ◽  
Radek Mikuláš ◽  
Petr Budil ◽  
Petr Kraft

Upper Ordovician shallow marine fine-grained sandstones and siltstones exposed in the Loděnice – vinice locality yielded a distinct and well-preserved tiering pattern of trace fossils. The two uppermost tiers are composed mainly of Bifungites and Nereites. Deeper in the sediment, tiers dominated by Thalassinoides, Zoophycos and Teichichnus occur. Most of the succession is completely bioturbated; however, several storm layers enabled study of a well-preserved frozen tiering pattern. Large portions of the bedding planes (ichnologic snapshots) showed a considerable patchiness of intensive surface bioturbation and a preferred orientation of Bifungites. The identified tiering pattern is one of the earliest examples of a well-documented complex tiering of burrows documented in detail.


Author(s):  
Štěpán Chládek ◽  
Pavel Uher ◽  
Milan Novák

Abstract We studied compositional variations in columbite group minerals (CGM) from several granitic pegmatites of the beryl-columbite subtype in the Maršíkov district, Silesian Domain of the Bohemian Massif, Czech Republic. The CGM are characterized by distinct zoned patterns in BSE images. Primary magmatic homogeneous to oscillatory zoning is preserved in corroded crystal cores, whereas the majority of the crystal volume is replaced by secondary complexly zoned domains formed via post-magmatic processes. The primary domains show relatively uniform evolutionary trends from core to rim, generally with steeply increasing Ta/(Ta + Nb) and negligible to slightly increasing Mn/(Mn + Fe). In contrast, the compositions of secondary CGM domains indicate a reversed evolution, with: (1) steeply decreasing Ta/(Ta + Nb) and relatively constant Mn/(Mn + Fe) characteristics for CGM in the Bienergraben and Scheibengraben pegmatites, and (2) insignificantly decreasing Ta/(Ta + Nb) and strongly decreasing Mn/(Mn + Fe) characteristics for CGM in the Schinderhübel I and Lysá Hora pegmatites. Patchy zoning and secondary evolution in CGM result from metasomatic replacement processes related to fluids. These fluids are probably late-magmatic and exsolved from the residual melt and in later stages locally mixed with external Mg-enriched fluids derived from the host rocks. The presence of volatiles (mainly H2O, F) facilitated high mobility of the elements and replacement of the early CGM. Textural characteristics and compositional variations in CGM show the complex evolution of the pegmatite system from the magmatic stage to subsolidus-hydrothermal conditions.


Clay Minerals ◽  
1998 ◽  
Vol 33 (2) ◽  
pp. 333-347 ◽  
Author(s):  
J. Colson ◽  
I. Cojan ◽  
M. Thiry

AbstractThe Danian of the Provence basin (SE France) is characterized by a strong subatmospheric alteration processes throughout the basin. A wide range of facies, depositional and weathering, were recognized in an interval of 5 Myr and include floodplain fine-grained alluvium, palustrine limestones, playa dolostones, mottled palaeosols, vadose and phreatic calcretes, and phreatic dolocretes. Palygorskite was invariably found in laminar, massive and honeycomb vadose calcretes and phreatic dolocretes, as well as in playa dolostones, and only exceptionally in floodplain siltstones, nodular calcretes and palustrine limestones. Regardless of the facies, palygorskite is associated with smectites. An authigenic origin, based on the morphology of the fibres and the vertical distribution of clay minerals, is proposed for palygorskites in all of the facies. The simultaneous occurrence of palygorskite in these environments is interpreted as a sign of a stable seasonal semi-arid climate and low detrital input during a period of low lake level (-0.5 Myr). The occurrence of authigenic palygorskite in siltstones around the lake was attributed to the rising of the water table, retention of the already saturated water in the pore spaces of the sediment, and its subsequent evaporation in a confined environment. A hydrogeological model is proposed for the distribution of palygorskite. The elongated shape of the Provence basin enhanced the influence of lateral inflow of freshwater during the low lake period which explains the distribution of palygorskite in different environments of the Provence basin as well as spatial distribution of phreatic calcretes and dolocretes. During the high lake level, palygorskite formed in the few remaining ephemeral ponds and on the floodplain along the lake margin.


2015 ◽  
Vol 15 (3) ◽  
pp. 111-124 ◽  
Author(s):  
Jana Kaiglová ◽  
Petr Jiřinec ◽  
Jakub Langhammer ◽  
Eva Ingeduldová ◽  
Dagmar Chalupová ◽  
...  

Blood ◽  
2016 ◽  
Vol 128 (22) ◽  
pp. 4125-4125
Author(s):  
Katerina Musilova ◽  
Gabriela Pavlasova ◽  
Vaclav Seda ◽  
Eva Vojackova ◽  
Katerina Cerna ◽  
...  

Abstract We and others have shown that deregulation of microRNAs (miRNAs) is associated with the biology of B cell malignancies, including regulation of B cell proliferation and survival (Musilova & Mraz, Leukemia, 2015). We focused on studying miRNAs that associate with the aggressiveness of FL and its transformation to diffuse large B cell lymphoma (DLBCL). First, we analyzed the expression of 380 miRNAs (TaqMan Arrays, ABI) in 8 paired primary samples of FL that subsequently transformed to DLBCL. We identified statistically significant changes (P<0.05, fold change >1.8) in the expression of 5 miRNAs. The most significant change was the down-regulation of miR-150 (~5 fold, P=0.01). Similarly, we observed significantly reduced miR-150 levels in an independent cohort of non-paired samples of FL before vs. after transformation to DLBCL, and miR-150 was significantly less expressed in de novo DLBCL in comparison with FL. MicroRNA miR-150 is of particular interest as we have shown that its expression determines BCR signaling propensity in chronic lymphocytic leukemia (CLL) B cells, and low levels associated with worse survival (Mraz et al., Blood, 2014). Therefore, we analyzed miR-150 expression in a cohort of 89 FL samples. We noticed that miR-150 expression was lower in samples from patients with a FLIPI score ≥3 (P=0.03), and with high Ki67 positivity (>20%; P=0.003). Moreover, FL patients with low miR-150 levels (<median) had significantly shorter survival (median survival 6.2 years vs. not reached; P=0.007; HR 3.0 [CI: 1.3-6.8]). To determine the potential reason for variable miR-150 levels in FL B cells, we tested the effect of microenvironmental interactions on its expression. In this experiment, a short term (48hrs) co-culture of B cell lymphoma cells with stromal cells (HS-5) led to down-regulation of miR-150 levels (P<0.05). Next we investigated the functional role of miR-150 by silencing its newly identified target, namely GAB1, in lymphoma B cells. The transfection of siGAB1 resulted in a significant reduction of BCR signaling after anti-IgM treatment (10ug/ml, assessed by calcium influx). We further showed that GAB1 is an adaptor molecule that allows for higher activity of the PI3K/AKT signaling pathway. CONCLUSION: Low miR-150 levels associate with a shorter overall survival in FL. This could be used as a reasonable prognostic marker since high miRNA stability allows reliable analyses of miR-150 levels from formalin-fixed, paraffin-embedded (FFPE) samples. Interactions with stromal cells and/or soluble microenvironmental factors down-modulate miR-150 levels in B cells, which support their BCR signalling potential. We are further investigating to what extent the miR-150 down-regulation is causally connected with the aggressiveness and/or transformation of FL. This work was supported by: the Ministry of Education, Youth and Sports of the Czech Republic under the project CEITEC 2020 (LQ1601); the European Union's Horizon 2020 research and innovation programme under grant agreement No. 692298; the research grant GACR (16-13334Y); the Ministry of Health of the Czech Republic, grant nr. 16-29622A. All rights reserved. This work was financed from the SoMoPro II Programme (project No. 4SGA8684), co-financed by European Union and the South-Moravian Region. This publication reflects only the author's views and the Union is not liable for any use that may be made of the information contained therein; Masaryk university as part of the project "New approaches in research, diagnostics and therapy of hematological malignancies III", number MUNI/A/1028/2015 with the support of the Specific University Research Grant, as provided by the Ministry of Education, Youth and Sports of the Czech Republic in the year 2016; the Ministry of Health of the Czech Republic - conceptual development of research organization (FNBr, 65269705, Sup 3/16); the Ministry of Education, Youth and Sports of the Czech Republic, grant nr. LD15144 (COST CZ); the research grant TACR (TEO2000058/2014-2019); and EHA Research Fellowship award granted by the European Hematology Association. G.P. is a city of Ostrava scholarship holder. Disclosures No relevant conflicts of interest to declare.


2008 ◽  
Vol 254 (3-4) ◽  
pp. 197-215 ◽  
Author(s):  
Michael J. Jercinovic ◽  
Michael L. Williams ◽  
Edward D. Lane

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