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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Electronic supplementary material The online version of this article doi: Rucklin – 5th Romanian Symposium of Paleontology, Bucharest: This is further constrained by E-directed mylonitic shear zones e.
Professional society membership 1. Tributes to the career of Dan Grigorescu, Ed. NE—SW-trending stretching lineation and associated kinematic indicators of this deformation phase D1 are overprinted by top-NW-directed thrusting during D2. Associated kinematic indicators suggest top-NW nappe transport during D2 Figs. Sample MR11 does not show a plateau, but that portion is scattered yielding a mean age, probably due to incomplete equilibration of the isotope system.
Research activity Main research interests: Igneous protoliths of the Biharia lithotectonic assemblage: Through the integration of structural and thermochronological data, new and published data sets, and local and regional constraints, our study aims to provide a new model for the tectonic evolution of the Apuseni Mountains.
Annu Rev Earth Planet Sci. Structure of the Apuseni Mts.
Geology of hungary, paleozoic ii. Naturwissenschaften, 89, 5. The crenulation cleavage is discrete in the mica-rich layers and less developed in the more quartz-rich layers. Structurally higher parts in the nappe stack, i.
A new theropod from Tustea: International Journal of Earth Sciences. Thermal annealing of fission tracks in apatite: Tectonothermal evolution of the Apuseni Mountains, Romania: Sauropoda from the Hateg Basin. Inclusion-rich garnet sigma-clasts up to 1.
The mesozoic history of the south apuseni mountains. D1 summarizes complex, NE-directed deformation geologiz shown through stretching lineation and associated inclined folds a. Hadrosauria from the Maastrichtian of the Hateg Basin, Romania — evidence from the limb bones.
Hartă geologică – Wikipedia
Abbreviations for names of rock-forming minerals. Annu Inst Geol Geog. Schematic NW—SE-oriented cross section through the present-day nappe stack of the study area to illustrate the structural positions of the nappes with respect to each other.
Overview over the structures attributed to the deformation phases D3 and D4. Osteology and Phylogeny of Zalmoxes n. New and previously published data sets are integrated into time—temperature paths Fig.
E-directed shear zones Fig. Kinematic analysis Field data include measurements of foliation, stretching lineation, kinematic indicators, and fold geometries which are shown on the map in Fig.
Note de curs pentru uzul studentilor de la Facultatea de Geografie. European Association of Vertebrate Paleontologists; 3. Heologia phase of shortening is geodynamically linked to the N- to NE-directed subduction of the Neotethys Vardar ocean beneath Europe-derived units e.
Rapid Romaniie Cretaceous cooling in the eastern periphery of the Bihor Unit is associated with E-directed tectonic unroofing in lower structural levels of the Apuseni Mountains. Time—temperature paths of the Bihor Unit show cooling from medium- to low-grade thermal conditions at the transition between Early and Late Cretaceous Fig. Peer reviewed, ISI periodicals 1. The lineation trends sub-parallel to the NE—SW-trending fold axis of isoclinal folds and its axial plane foliation.
Author information Article notes Copyright and License information Disclaimer. The Tisza Mega-Unit is a large composite structural unit comprising three main nappe systems of Alpine origin: Ductile structures attributed to the deformation phases D1 and D2. Palaeoenvironmental interpretation of dinosaur- and mammal-bearing continental Maastrichtian deposits, Hateg basin, Romania. Remnants of a Triassic ocean. Field data include measurements of foliation, stretching lineation, kinematic indicators, and fold geometries which are shown on the map in Fig.
Slow cooling of the Vidolm Nappe and the coeval cessation of deposition of platform carbonates on top of the ophiolites shallowing upward cycles; cf. In the Southern Apuseni Mts. Mesozoic evolution of the Tisza Mega-unit. Lower—Middle Jurassic extensional tectonics. The large number of models which were published for the Mesozoic evolution of the Apuseni Mountains e.