인공고관절의 세라믹 볼 헤드의 기계적 안정성 평가를 위한 3 차원 유한요소 해석

A review on the adsorption of heavy metals by clay minerals, with special focus on the past decade

A correlation of tectonic units of the Alpine-Carpathian-Dinaridic system of orogens, including the substrate of the Pannonian and Transylvanian basins, is presented in the form of a map. Combined with a series of crustal-scale cross sections this correlation of tectonic units yields a clearer picture of the three-dimensional architecture of this system of orogens that owes its considerable complexity to multiple overprinting of earlier by younger deformations.

/pdf/the-alpine-carpathian-dinaridic-orogenic-system-correlation-2gm3qeefzn.pdf

The Alpine-Carpathian-Dinaridic orogenic system: correlation and evolution of tectonic units

The new tectonic map of the Alps is based on the combination of purely structural data with criteria regarding paleogeographical affiliation and/or tectono-metamorphic evolution. The orogenic evolution of the Alps is discussed using a combination of maps and paleogeographical reconstructions. It is proposed that the Alps are the product of two orogenies, a Cretaceous followed by a Tertiary one. While the former is related to the closure of an embayment of the Meliata ocean into Apulia, the latter is due to the closure of the Alpine Tethys between Apulia and Europe. The along-strike changes in the overall architecture, as for example revealed by geophysical-geological transects, are by far more substantial than hitherto believed. It appears that the Alps are still far from being over-investigated, as is demonstrated by many surprising recent findings based on field geology, laboratory results and geophysical methods of deep sounding.

/pdf/tectonic-map-and-overall-architecture-of-the-alpine-orogen-23efh3jp0j.pdf

Tectonic map and overall architecture of the Alpine orogen

/pdf/reconciling-plate-tectonic-reconstructions-of-alpine-tethys-1do3i5vm2t.pdf

Reconciling plate-tectonic reconstructions of Alpine Tethys with the geological–geophysical record of spreading and subduction in the Alps

Alpine metamorphism of the Eastern Alps

Tectonic significance of the geochemistry and petrology of ophiolites in southeast Anatolia, Turkey

Metamorphic Structure of the Alps.

Andean-type active margin formation in the eastern Taurides: Geochemical and geochronogical evidence from the Baskil granitoid (Elazığ, SE Turkey)

The Kizildag (Hatay) ophiolite is one of the best preserved Neotethyan oceanic lithospheric remnants in southern Turkey. It is represented by, from bottom to top, mantle tectonites, ultramafic to mafic cumulates, isotropic gabbros, sheeted dike complex, plagiogranites and extrusives (low-K tholeiites and boninites). The ultramafic to mafic cumulate rocks are composed of dunite, wehrlite, olivine gabbro, olivine gabbronorite and gabbro. The crystallization order of cumulus phases, and the presence of highly magnesian olivines and pyroxenes as well as highly calcic plagioclases in the cumulates, indicate a subduction-related tectonic environment and suggest derivation from an island arc tholeiitic magma. The isotropic gabbros are represented by gabbro, diorite and quartz diorite with granular, ophitic to micrographic textures. The sheeted dikes are characterized by diabase and microdiorite with ophitic to intersertal textures. The boninitic volcanics (so-called sakalavites) are basaltic in composition and exhibit hypocrystalline porphyric to hyalopilitic textures. All these rocks are tholeiitic in composition. New geochemical data presented in this paper from the isotropic gabbros, sheeted dikes and sakalavites suggest that there are two main types of parental basic magmas that form the crustal rocks of the Kizildag (Hatay) ophiolite. These are (i) IAT series comprising the Group I isotropic gabbros and sheeted dikes; (ii) Low-Ti boninitic series characterized by the Group II isotropic gabbros, sheeted dikes and sakalavites. The spatial and temporal relations of the IAT and boninitic magma types in the Kizildag ophiolite indicate that different magma sources were contemporaneously active in a fore-arc tectonic setting of the southern branch of Neotethys during the Late Cretaceous.

/pdf/geochemistry-and-tectonic-environment-of-diverse-magma-1k8kj4sq5o.pdf

Geochemistry and Tectonic Environment of Diverse Magma Generations Forming the Crustal Units of the Kızıldağ (Hatay) Ophiolite, Southern Turkey

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