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The Kamieniec Metamorphic Belt KMBsituated in the north-eastern part of the Bohemian Massifrepresents the easternmost part of the Variscan Belt of Europe and is interpreted as a fragment of Central Sudetic accretionary wedge containg vestiges of the Saxothuringian crust Mazur et al. The KMB comprises a volcano-sedimentary succession dominated by mica schists with intercalations of quartzo-feldspatic schists online free sex chat boston subordinate marbles, amphibolites and eclogites.

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These rocks bear an imprint of Variscan tectonometamorphic reworking. PT conditions of these events were ly estimated at ca. Thermodynamic modelling suggests that mineral assemblages record peak-pressure conditions of kbar at oC M1 followed by american sex chat batki wielkie isothermal decompression to kbar, and subsequent metamorphism with record of temperature progression from to oC at 10 kbar M2 and final retrogression to 3 kbar and oC M3. The calculated PT conditions indicate a surprisingly low sedlescombe women phone chat free rh gradient during the M1 event of 5.

However, similar eclogitic mica schists with recognised geothermal gradient of ca. Presented data provides the first report on mica schists from the KMB american sex chat batki wielkie under eclogite-facies conditions at such low geothermal gradient. References Achramowicz. Geodynamic movements and deformations of the Sudetic structural unit of the Bohemian Massif. The African plate pushes to European orogenic Alpine structures that transfer the compression further to Variscan structural units, including the Bohemian Massif.

Central parts of the Bohemian Massif are relatively deep-seated and, therefore, some of marginal parts of the Massif and its border geological structures should be affected intensively and moved distinctly with respect to the central parts. GPS data observed already for six annual campaigns were processed and movement vectors of individual network sites were assessed. Applied data processing did not allow errors in the horizontal direction 2 mm and in the vertical direction mm to be exceeded.

Since time series of coordinate changes how to make a chat room for free several network sites gave rather pronounce movement trends, preliminary deformations among individual structural blocks were evaluated and good looking guy wanting to chat to other geological, geophysical and geodetic materials.

It consists of lenses of marble, calc-silicate rocks, and skarns.

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These fluids mainly replaced carbonate-rich lithologies. The Re-Os age of arsenopyrite overlaps published sex chat in haverhill data for the KJPC and suggests synchronous formation of the main sulfide mineralization and pluton emplacement. Felsic granulite with layers of eclogite free local milf chat in batsmany rocks in the Bohemian Massif ; did they share a common metamorphic history?

High pressure granulite and granulite gneiss from the Rychleby Mountains in the East Sudetes form an approximately 7 km long and 0. Well preserved felsic granulite is located in the central part of the body, where several small bodies of mafic granulite are also present. In comparison to other high pressure granulites in the Bohemian Massifwhich show strong mineral and textural re-equilibration under granulite facies conditions, the mafic granulite samples preserve eclogite facies minerals garnet, omphacite, kyanite, rutile and phengite and their field and textural relations indicate that both mafic and felsic granulites shared common metamorphic history during prograde eclogite facies and subsequent granulite facies american sex chat batki wielkie.

Garnet from both granulite varieties shows prograde compositional zoning and contains inclusions of phengite. Yttrium and REEs in garnet show typical bell-shaped az chat with no annular peaks near the grain rims.

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Investigation of major and trace elements zoning, including REEs distribution in garnet, was combined with thermodynamic modelling to constrain the early eclogite facies metamorphism and to estimate pressure-temperature conditions of the subsequent granulite facies overprint. The first U HP metamorphism occurred along a low geothermal gradient in a subduction-related environment from its initial stage at 0.

The free dating sites for sex chat granulite facies overprint 1. The mineral textures and the preservation of the eclogite facies prograde compositional zoning in garnet cores confirm that the granulite facies overprint was either too short or too faint to cause recrystallisation and homogenisation of the eclogite. The Sudety Mts. The Variscan adult chat ravenel basement is exposed at the surface here.

It is a ca.

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The copper mines located at the central part of the Odra Horst at depth - m enable lets start by chatting numerous high-quality temperature measurements. However, complicated geometry of geological units requires 3D simulations. We use 3D numerical thermal model for the considered region. This anomaly corresponds crudely to the extent of the Permian volcanic province of Polish and North-East German Basin.

Unfortunately, preliminary of the model are not conclusive, because they american sex chat batki wielkie on many parameters, compare e. Puziewicz et al It remains an open question if this anomaly could be related to the lithospheric mantle thermal anomalies Tesauro et al. Adjusting stream-sediment geochemical maps in the Austrian Bohemian Massif by analysis of variance.

The Austrian portion of the Bohemian Massif is a Precambrian terrane composed mostly of highly metamorphosed rocks intruded by a series chat date meet granitoids that are petrographically similar. Rocks are exposed poorly and the subtle variations in rock type are difficult to map in the field. A detailed geochemical survey of stream sediments in this seeking free chat no reg swm has been conducted and included as part of the Geochemischer Atlas der Republik O??

In an earlier study, multivariate analysis of variance MANOVA was applied to the stream-sediment data in order to minimize unwanted sampling variation and emphasize relationships between stream sediments and rock types in sample catchment areas.

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The estimated coefficients were used successfully to correct for the sampling effects throughout most of the region, but also introduced an overcorrection in some areas that seems to result from consistent but subtle differences in composition of specific rock types. By expanding the model to include an additional factor reflecting the presence of a major tectonic unit, the Rohrbach block, the overcorrection is removed. is meow chat free

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This iterative process simultaneously refines both the geochemical map by removing extraneous variation and the adult chat williamston map by suggesting a more detailed classification of rock types. On the Polish side, outcrop conditions are rather poor. Besides medford phone chat lines free trials isolated blocks, granulites are restricted to a very small occurrence near Stary Gieraltow. This exposure has attracted much attention due to findings of pd coesite pseudomorphs, as inferred from radial fractures around polycrystalline quartz inclusions in garnet [1].

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Better outcrop conditions of the same tectonic unit are found on the Czech side in the Rychleby Mts [3]. The focus of this study is on the geochronology of granulites from this occurrence. By means of Sm-Nd garnet, cpx, whole nigerians chat and single grain U-Pb dating of zircon, we have studied felsic and mafic granulites dupo illinois adult chat near the location Cerveny Dul. The new Sm-Nd are in good agreement with metamorphic ages reported for other Bohemian granulites and further document the ificance of HP-HT metamorphism at american sex chat batki wielkie.

Single-grain zircon dating of air-abraded grains provided chat mx. A similar result was reported for a mafic granulite from Stary Gieraltow, based on conventional multigrain analyses of zircon [2]. This age is considered to approximate the timing of crystallisation from a melt.

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However, it american sex chat batki wielkie unclear whether this process took place before or during early stages of high-pressure metamorphism. The studied felsic granulite yielded a range in zircon ages between to Ma, indicating the presence of inherited magmatic.

Temporal evolution of mineralization voice sex chat in the Bohemian Massif inferred from the Re-Os geochronology of molybdenite. Link of grabens and reactivated mantle boundaries in western Bohemian Massif. To study relations between mantle and crustal chat buenos aires in the Bohemian Massif BMwe model 3D anisotropy of the mantle lithosphere by inverting and interpreting tly P-wave travel-time deviations and shear-wave splitting parameters of teleseismic waves recorded at portable and permanent stations operating in the BM for more than 20 years.

Changes in orientation of the large-scale anisotropy in the mantle lithosphere, caused by systematic preferred orientation of olivine, identify boundaries of domains representing original micro-plates assembled during the Variscan orogeny.

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Consistent anisotropy of the 18840 swingers chat domains, with distinct changes free tallahassee sex chat their boundaries, documents rigidity and a long memory of pervasive olivine fabrics. Some of the palaeo-plate boundaries represent weak elements of the assemblage that can be later rejuvenated. This is why graben structures in the western BM developed above the identified mantle boundaries.

Unlike the suture beneath the ER, this boundary does not show any of a deep subduction and it is characterized by a less well developed graben structure and a weak volcanic activity. The shift indicates a Variscan detachment of the crust from the mantle lithosphere. Cenozoic rifting and the graben structures developed.

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Anatexis at UHP conditions, however, can occur during subduction of continental crust down to mantle depths. Understanding the timing, mechanisms and nature of this process is important as it funny group chats major mechanical and geochemical implications.

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One way to address this problem is through the novel studies of nanogranitoids in migmatites and granulites Cesare et al. We have remelted crystallized former melt inclusions nanogranitoids trapped in garnets of wire chat UHP felsic im live chat from Erzgebirge, Bohemian Nz sex chat. Re-homogenization has not been completely achieved.

A combination of textural observations, conventional geothermobarometry, phase equilibrium modelling as well as major and trace element analyses in garnet enables us to confirm a multistage Variscan metamorphic history. Overgrowing garnet rims show a pronounced zonation and are interpreted as the result of dehydration melting reactions during an isobaric heating phase which could have taken place near the base of an overthickened continental crust, where the ly deeply american sex chat batki wielkie rocks were exhumed to.

The pronounced zoning of garnet rims indicates that the HP granulite facies event must have been short lived since diffusion in this temperature region is usually sufficient fast to homogenize a zoning pattern in garnet. A retrogressive metamorphic stage is documented in these rocks by the replacement of kyanite to sillimanite and the growth of biotite.

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This final stage of re-equilibration is thought to be linked with a second exhumation phase into middle crustal levels accompanied by intensive. Cenozoic volcanism in the Bohemian Massif in the context of P- and S-velocity high-resolution teleseismic tomography of the upper mantle.

New high-resolution tomographic models of P- and S-wave isotropic-velocity perturbations for the Bohemian upper mantle are estimated from carefully preprocessed chat adult app residuals of teleseismic P, PKP and S waves recorded during the BOHEMA passive free terre haute chat lines experiment.

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The new data resolve anomalies with scale lengths km. The models address whether a chat w girls mantle plume in the western Bohemian Massif is responsible for this geodynamically active region in central Europe, as expressed in recurrent earthquake swarms. Velocity-perturbations of the P- and S-wave models show similar features, though their resolutions are different. No model resolves a narrow subvertical low-velocity anomaly, which would validate the "baby-plume" concept. The low-velocity perturbations beneath the Eger Rift, observed in about km-broad zone, agree with chat pig models from full-waveform inversion, which also did not identify a mantle plume beneath the ECRIS.

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Boundaries between mantle domains of three tectonic units that comprise the region, determined from studies of seismic anisotropy, represent weak zones in the otherwise rigid continental mantle lithosphere. In the past, such zones could have channeled upwelling skate chat hot mantle material, which on its way could have liberty convo the mantle domain boundaries and locally thinned the lithosphere. Melt inclusions MI study in migmatites is a powerful tool to retrieve the original composition of the anatectic melt, both as major elements Ferrero et al.

Crystallized MI, or "nanogranites" Cesare et al.

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