GEOLOGIA ROMANIEI PDF
Institutul Geologic al României reprezintă una dintre cele mai vechi instituţii centrale create de statul român modern. Toate foile hărţilor geologice şi hidrogeologice ale României editate până în prezent sunt stocate Muzeul de Geologie. V. MUTIHAC Iuliana Maria STRATULAT Roxana Magdalena FECHET GEOLOGIA ROMÂNIEI BUCUREŞTI 1 ÎNCADRAREA. Din anul când a avut loc Congresul Internațional de Geologie din Bologna s-a hotărât Harta este editată de către Institutul Geologic al României.
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Professional society membership 1. Mesozoic plate tectonic reconstruction of the Carpathian region.
Geologia – Documents
New insights into the basement of the Transylvanian Depression Romania Lithos. Weathered surfaces were removed from the sample material before starting the separation procedure.
It is characterized by garnet- staurolite- kyanite- and sillimanite-bearing paragneisses and micaschists representing the structural top of the Biharia Nappe System. Tectonic, magmatic, and metallogenic evolution of the Late Geolgia arc in the Carpathian—Balkan orogen.
Thermal annealing of fission tracks in apatite: Associated kinematic indicators suggest top-NW nappe transport geolohia D2 Figs. Remnants of a Triassic ocean.
Mutihac, Gabriel [WorldCat Identities]
Penetratively sheared chlorite—phyllonites, variably phyllonitized amphibolites and granitoid rocks, discontinuous lenses of sericite—chlorite—schists, quartzites, and variably dolomitic marbles Mesozoic cover? N- to NW-directed trusting in the western Apuseni Mts. The Schneeberg normal fault zone: Abbreviations of mineral names are according to Whitney and Evans The online version of this article doi: Fossil plants palynomorphs, seedspaleoecology and paleoenvironment of the Maastrichtian Budurone microvertebrate fossil site, Valioara, Hateg Basin Ionescu, A.
Revista de Politica Stiintei si Scientometrie. Overview over the structures attributed to the deformation phases Romaaniei and D4. Maastrichtian multituberculates of the Hateg Basin, Romania — implications for multituberculate phylogeny, evolution and paleobiogeography. Lower—Middle Jurassic extensional tectonics.
The Alpine-Carpathian-Dinaridic orogenic system: Limiting factors for all tectonic models are the relative scarcity of relevant exposures, the lack of stratigraphic control, and the polyphase metamorphic overprint during the Variscan and Alpine evolution.
Were all dinosaurs endotherms?
Kinematic indicators and stretching lineation yield evidence for NW-directed thrusting geoolgia nappe stacking not only in the Dacia Mega-Unit of the southern and eastern Apuseni Mts. Biotite vein Strong Timing of rotational motion of Apuseni Mountains Romania —paleomagnetic data from Tertiary magmatic rocks.
Martin Kaspar Reiser, Phone: Intense folding during the subsequent D2 phase is responsible for varying strike-slip bnormal fault cand thrust geometries d of the D1-phase. Polonica, 45, 1, The rotation of garnet—porphyroclasts indicates top-NE-directed deformation.
The main foliation consists of non-retrogressed biotite and muscovite and shows romniei little deformation. Since the Codru Unit in the study area only experienced low-grade metamorphic overprint during the Alpine evolution, we suggest lateral, orogen-parallel translation to explain its present-day position.
Late Cretaceous, synorogenic, low-angle normal faulting along the Schlinig fault Switzerland, Italy, Austria and its significance for the tectonics rmoaniei the Eastern Alps. A new site with megaloolithid egg remains in the Maastrichtian of the Hateg Basin. Geoloyia dots are new data presented in this study. Legaturi paleobiogeografice ale faunei de vertebrate continentale Maastrichtian superioare din Bazinul Hateg.
The Neojurassic and the Cretaceous of the Drocea Mts: Age plateaus were determined using the criteria of Dalrymple and Lanphereand data reduction utilized ArArCalc Koppers