Search results for "GEOLOGY"

showing 10 items of 6012 documents

Geology of the Bozdag area, central Menderes massif, SW Turkey: Pan-African basement and Alpine deformation

1998

The Menderes massif consists of a Precambrian Core Series that preserves evidence for a polymetamorphic history and a Paleozoic/Mesozoic Cover Series that experienced only the Alpine tectonometamorphic evolution. Structural, petrographic, and geochronologic investigations in the central Menderes massif demonstrate that (a) part of the metamorphic and structural evolution of the Precambrian basement is older than the undeformed 551+/-1.4-Ma-old Birgi metagranite, and (b) inferred Alpine fabrics overprinting the Cover Series largely have the same attitudes as the old structures in the much older Core Series. The inferred Alpine fabrics include both contractional and extensional structures. Co…

geographygeography.geographical_feature_categoryGreenschistGeochemistry550 - Earth sciencesMassifImbricationPrecambrianBasement (geology)General Earth and Planetary SciencesShear zoneStructural geologyGeomorphologyGeologyMetamorphic faciesGeologische Rundschau
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Structural and thermal history of poly-orogenic basement: U-Pb geochronology of granitoid rocks in the southern Menderes Massif, Western Turkey

2004

Ion microprobe U-Pb dating of granitoid rocks from key structural outcrops of the Menderes Massif in western Turkey provides an important constraint to the thermal and deformational history of a structurally complex metamorphic belt within the Alpine chain. Crystallization ages of two granite protoliths, derived from the weighted means of rim ages and the ages of homogeneous prismatic zircon grains, are 541 +/- 14 Ma and 566 +/- 9 Ma, whereas the cores of zoned pyramidal and short-prismatic zircon grains range from Palaeoproterozoic to Neoproterozoic in age. These ages indicate that amphibolite- to gramilite-facies metamorphic rocks in much of the Menderes Massif were deformed, metamorphose…

geographygeography.geographical_feature_categoryGreenschistGeochemistryGeologyMassifBasement (geology)GeochronologyAlpine orogenyPetrologyProtolithMetamorphic faciesGeologyZircon
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Structures along the Orobic thrust, Central Orobic Alps, Italy

1997

A series of regional deformation phases is described for the metamorphic basement and the Permian cover in an area in the central Orobic Alps, northern Italy. In the basement deformation under low-grade amphibolite metamorphic conditions is followed by a second phase during retrograde greenschist conditions. These two phases predate the deposition of the Permian cover and are of probable Variscan age. An extensional basin formed on the eroded basement during the Late Carboniferous, filled with fan conglomerates and sandstones, and rhyolitic volcanic rocks. Well-preserved brittle extensional faults bound these basins. Further extension deformed basement and cover before the onset of Alpine c…

geographygeography.geographical_feature_categoryGreenschistInversion (geology)GeochemistryNappeVolcanic rockTectonicsAlpine orogenyGeneral Earth and Planetary SciencesThrust faultStructural geologyGeologySeismologyGeologische Rundschau
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Aspects of the kinematic history and mechanisms of superposition of the proterozoic mobile belts of eastern Central Africa (northern Malawi and south…

1993

Abstract Commonly the Proterozoic tectonic evolution of the Central African basement is subdivided into three major events: (1) the Ubendian (∼2300−1800 Ma), (2) the Irumide (∼1350−950 Ma), and (3) the Pan-African (∼900−450 Ma) orogenic cycles. Relics of the Ubendian event are granite intrusions and, possibly, an amphibolite- to granulite-facies metamorphism. The Ubendian orogeny was followed by deposition of clastic sediments (Muva supergroup). In northern Malawi these sediments and the underlying basement were then thrust to the east-southeast/southeast during the Irumide orogeny. Horizontal shearing along subvertical zones (i.e. the Ubendian belt) was associated with subhorizontal crusta…

geographygeography.geographical_feature_categoryGreenschistProterozoicGeochemistryMetamorphismGeologyOrogenyCratonGeochemistry and PetrologyThrust faultShear zoneMetamorphic faciesGeologyPrecambrian Research
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Generation of early Archaean grey gneisses through melting of older crust in the eastern Kaapvaal craton, southern Africa

2014

Abstract We report zircon ages, Hf-in-zircon isotopes as well as whole-rock geochemistry and Hf–Nd isotopic systematics for Palaeoarchaean grey gneisses of the Ancient Gneiss Complex of Swaziland, the oldest components of the Kaapvaal craton, southern Africa. The Hf-in-zircon isotopic compositions in these compositionally heterogeneous, multicomponent, migmatitic gneisses are highly variable, even in the oldest zircons dating back to 3.66 Ga, suggesting growth of zircon from melts representing a mix of juvenile and anatectic material derived from differentiated continental crust of Eoarchean to late Hadean age. In contrast, the initial Nd and Hf whole-rock isotopic compositions are frequent…

geographygeography.geographical_feature_categoryHadeanContinental crustArcheanCrustal recyclingPartial meltingGeochemistryGeologyCratonGeochemistry and PetrologyGeologyZirconTerranePrecambrian Research
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Late-glacial to Holocene aeolian deposition in northeastern Europe - The timing of sedimentation at the Iisaku site (NE Estonia)

2015

Abstract The Late-glacial and Holocene aeolian inland dune complex at Iisaku (NE Estonia) has been investigated using an accurate and detailed compilation of the sedimentary properties and chronological framework. The quartz grains forming the dunes are very variable, reflecting aeolian, weathering, and periglacial conditions, both prior and after deposition. Although the morphological forms and the sedimentary record point to a dune-like environment, the transport record reflects either a short transport time or/and distance, and a contribution from neighbouring sedimentary environments. Dune development in the area was strongly controlled by the formation of the Baltic Ice Lake (BIL) in f…

geographygeography.geographical_feature_categoryHoloceneInland dunesGlacierLate-glacialPaleontologyOptically stimulated luminescence datingSedimentary featuresAeolian processesSedimentary rockYounger DryasGlacial periodGeomorphologyDeposition (chemistry)GeologyHoloceneEarth-Surface ProcessesChronology
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H2S fluxes from Mt. Etna, Stromboli, and Vulcano (Italy) and implications for the sulfur budget at volcanoes

2005

Abstract We present here new measurements of sulfur dioxide and hydrogen sulfide emissions from Vulcano, Etna, and Stromboli (Italy), made by direct sampling at vents and by filter pack and ultraviolet spectroscopy in downwind plumes. Measurements at the F0 and FA fumaroles on Vulcano yielded SO 2 /H 2 S molar ratios of ≈0.38 and ≈1.4, respectively, from which we estimate an H 2 S flux of 6 to 9 t · d −1 for the summit crater. For Mt. Etna and Stromboli, we found SO 2 /H 2 S molar ratios of ≈20 and ≈15, respectively, which combined with SO 2 flux measurements, suggest H 2 S emission rates of 50 to 113 t · d −1 and 4 to 8 t · d −1 , respectively. We observe that “source” and plume SO 2 /H 2 …

geographygeography.geographical_feature_categoryHydrogen sulfidechemistry.chemical_elementMineralogySulfurFumarolePlumechemistry.chemical_compoundFlux (metallurgy)chemistryImpact craterVolcanoGeochemistry and PetrologySulfur dioxideGeologyGeochimica et Cosmochimica Acta
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Continuous monitoring of hydrogen and carbon dioxide at Mt Etna

2013

article i nfo This study assessed the use of an H2 fuel cell as an H2-selective sensor for volcano monitoring. The resolution, repeatability, and cross-sensitivity of the sensor were investigated and evaluated under known laboratory conditions. A tailor-made device was developed and used for continuously monitoring H2 and CO2 at Mt Etna throughout 2009 and 2010. The temporal variations of both parameters were strongly correlated with the evolution of the volcanic activity during the monitoring period. In particular, the CO2 flux exhibited long-term variations, while H2 exhibited pulses immediately before the explosive activity that occurred at Mt Etna during 2010.

geographygeography.geographical_feature_categoryHydrogenContinuous monitoringCo2 fluxchemistry.chemical_elementSoil CO2 fluxH2 monitoringH2 fuel cell Mt EtnaGeologyRepeatabilityAtmospheric sciencesSettore GEO/08 - Geochimica E VulcanologiaSoil co2 fluxchemistry.chemical_compoundVolcanochemistryGeochemistry and PetrologyCarbon dioxideFuel cellsSeismologyGeologyChemical Geology
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Intercomparison of volcanic gas monitoring methodologies performed on Vulcano Island, Italy

2004

[1] Volcanic gas emissions from fumaroles on the rim of La Fossa crater, Vulcano Island, Italy, were measured simultaneously using direct sampling (for H2O, CO2, total sulfur, HCl and HF), filter packs (for SO2, HCl, HF) and short-path active-mode FTIR measurements (for H2O, CO2, SO2, HCl and HF) in an intercomparison study in May 2002. The results show that Cl/F ratios were in good agreement between all three methods, and that FTIR and direct sampling determined comparable proportions of CO2 and H2O. Amounts of total S observed in direct sampling data were approximately double the amounts of SO2 measured with filter packs and FTIR. This difference could be attributed either to the fact FTI…

geographygeography.geographical_feature_categoryInfrared spectroscopychemistry.chemical_elementMineralogySulfurFumarolechemistry.chemical_compoundGeophysicsVolcanochemistryImpact craterGeneral Earth and Planetary SciencesSublimation (phase transition)Fourier transform infrared spectroscopySulfur dioxideGeologyGeophysical Research Letters
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Tunable diode laser measurements of hydrothermal/volcanic CO<sub>2</sub> and implications for the global CO<sub&am…

2014

Abstract. Quantifying the CO2 flux sustained by low-temperature fumarolic fields in hydrothermal/volcanic environments has remained a challenge, to date. Here, we explored the potential of a commercial infrared tunable laser unit for quantifying such fumarolic volcanic/hydrothermal CO2 fluxes. Our field tests were conducted between April 2013 and March 2014 at Nea Kameni (Santorini, Greece), Hekla and Krýsuvík (Iceland) and Vulcano (Aeolian Islands, Italy). At these sites, the tunable laser was used to measure the path-integrated CO2 mixing ratios along cross sections of the fumaroles' atmospheric plumes. By using a tomographic post-processing routine, we then obtained, for each manifestati…

geographygeography.geographical_feature_categoryInfraredStratigraphyPaleontologySoil ScienceMineralogyGeologyGeophysicsHydrothermal circulationFumaroleGeophysicsVolcanoImpact crater13. Climate actionGeochemistry and PetrologyContour lineAeolian processesTunable laserGeologyEarth-Surface ProcessesSolid Earth
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