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Evaluation Of Pgaa Data For Provenance Of Lithic Artifacts, Otis N. Crandell Dec 2011

Evaluation Of Pgaa Data For Provenance Of Lithic Artifacts, Otis N. Crandell

Studia UBB Geologia

The objectives of the study were to determine whether Prompt Gamma Activation Analyses (PGAA) could be successfully used to trace the source(s) of various Neolithic artifacts made of microcrystaline quartz. Two macroscopically identical sources of jasper from central and western Romania were analyzed by PGAA along with five Neolithic artifacts from the Limba site (Alba County). Due to the limited number of trace elements, which can be measured by PGAA, this method when used alone might produce inconclusive results for discriminating between jaspers from different sources. The interpretation of the data may be used for general assessments of provenance involving …


2011 Percival Allen Medal Award, Corina Ionescu, Tudor Berza Nov 2011

2011 Percival Allen Medal Award, Corina Ionescu, Tudor Berza

Studia UBB Geologia

The Association of European Geological Societies (AEGS) connects geological societies all over Europe. In 2006, the AEGS Executive Committee established an award named for Prof. Percival Allen FRS, one of the AEGS's founders. This medal is given biennially to a geoscientist for outstanding achievements in the field of international relations in Earth Sciences. Other than a distinguished record in fostering international relations in geosciences, there are no special eligibility criteria. The Award Committee announces the laureate at the Meetings of AEGS (MAEGS).

Dr. Jens Dieter Becker-Platen from Germany (at MAEGS-15, held in Tallinn 2007) and Dr. Eduardo de Mulder from …


Agglutinated Foraminifera From The Northern Tarcău Nappe (Eastern Carpathians, Romania), Raluca Bindiu, Sorin Filipescu Oct 2011

Agglutinated Foraminifera From The Northern Tarcău Nappe (Eastern Carpathians, Romania), Raluca Bindiu, Sorin Filipescu

Studia UBB Geologia

The Tarcău Nappe is the most important unit of the Carpathian flysch due to its size, stratigraphic, and tectonic complexity. Our purpose was to identify the major types of foraminifera assemblages in relation to the paleoenvironmental settings and their biostratigraphic potential. The identified assemblages are characteristic to the Cretaceous and Paleogene, consisting mostly of benthic agglutinated and, in lower proportions, benthic calcareous and planktonic species. Local abundances of Glomospira specimens allowed the correlation of the examined strata to the early Eocene “Glomospira event” described from the Carpathians in Poland, Morocco, and Labrador. Rzehakina fissistomata (Grzybowski) identified at Palma makes …


Effects Of Sediment Mineralogy To High-Iron Content In The Groundwater Of Rrogozhina Aquifer (Western Albania), Arjan Beqiraj, Enkeleida Beqiraj Oct 2011

Effects Of Sediment Mineralogy To High-Iron Content In The Groundwater Of Rrogozhina Aquifer (Western Albania), Arjan Beqiraj, Enkeleida Beqiraj

Studia UBB Geologia

The groundwater of Rrogozhina aquifer (western Albania) is generally characterized by high iron contents. Its water-bearing medium consists of soft to hard sandstone and conglomerate with intercalations of impermeable clay layers. The groundwater of Rrogozhina aquifer, that extends over a surface of 2100 km2 in the pre-Adriatic depression of Albania, occurs under typically artesian conditions. The iron content in ground water ranges from 0.2% up to 2.5%, but most of them fall within the interval 0.5-1.0 %. In groundwater iron occurs as reduced divalent ferrous iron (Fe+2) which is conditioned by the lack of water exposure to …


Experimental Techniques For Cement Hydration Studies, Andreas Luttge Oct 2011

Experimental Techniques For Cement Hydration Studies, Andreas Luttge

Studia UBB Geologia

Cement hydration kinetics is a complex problem of dissolution, nucleation and growth that is still not well understood, particularly in a quantitative way. While cement systems are unique in certain aspects they are also comparable to natural mineral systems. Therefore, geochemistry and particularly the study of mineral dissolution and growth may be able to provide insight and methods that can be utilized in cement hydration research. Here, we review mainly what is not known or what is currently used and applied in a problematic way. Examples are the typical Avrami approach, the application of Transition State Theory (TST) to overall …


Geomathematical Characterisation Of The Mineralization Indicators: A Case Study From Tincova Magmatic Intrusion (Romania), George Tudor Sep 2011

Geomathematical Characterisation Of The Mineralization Indicators: A Case Study From Tincova Magmatic Intrusion (Romania), George Tudor

Studia UBB Geologia

Indicators of the hydrothermal mineralization in the Tincova Laramian intrusion were tested at the contact zone between the intrusive body and the metamorphic host rocks. The mineralization consists of Cu, Pb and Zn sulfides, arsenopyrite, pyrrhotite and pyrite in gangue of quartz, carbonates, feldspar, sericite or clay minerals, and includes areas of hydrothermal alteration or oxidation. Seventy-nine samples were analyzed and processed as two distinct populations. Geomathematical methods highlight the importance of factors such as the shape, sizes of the mineralized zones and geological processes involved in the ore genesis. Trend maps for Cu, Pb + Zn, and Ag interpolated …


About A Peri-Gondwanan-North African Enlarged Acceptance Of The Caledonian Orogeny, Ioan Balintoni, Constantin Balica, Horst-Peter Hann Apr 2011

About A Peri-Gondwanan-North African Enlarged Acceptance Of The Caledonian Orogeny, Ioan Balintoni, Constantin Balica, Horst-Peter Hann

Studia UBB Geologia

The notion of “Caledonian Orogeny” is restricted by most authors to the Ordovician-Devonian thermotectonic events associated with the Laurentia-Baltica- Avalonia suturing. However, some views consider an orogeny as the sum of tectonic, metamorphic and magmatic events accompanying an entire supercontinent assembly or Wilson cycle. Following this line of thinking, the Caledonian and Variscan orogenies successively assembled Pangea. During the Ordovician Period, rifting, collision, deformation, metamorphism and magmatism took place within the Gondwana margin. All these events are known today in the basement of the Cadomian terranes from Iberia through the Alps up to the Romanian Carpathians and Balkans. We plead …


In Memoriam, Lukas Plan, Michele Citterio Apr 2011

In Memoriam, Lukas Plan, Michele Citterio

Studia UBB Geologia

In Memoriam - Willi Dansgaard & Robert Seemann


State Of The Art And Challenges In Cave Minerals Studies, Bogdan P. Onac, Paolo Forti Apr 2011

State Of The Art And Challenges In Cave Minerals Studies, Bogdan P. Onac, Paolo Forti

Studia UBB Geologia

The present note is an updated inventory of all known cave minerals as March 2011. After including the new minerals described since the last edition of the Cave Minerals of the World book (1997) and made the necessary corrections to incorporate all discreditations, redefinitions, or revalidation proposed by the Commission on New Minerals, Nomenclatures and Classification (CNMNC) of the International Mineralogical Association (IMA), we summed up 319 cave minerals, many of these only known from caves. Some of the minerals building up speleothems are powerful tracers of changes in Quaternary climate, other minerals are useful for reconstructing landscape evolution, or …


New Data On The Upper Jurassic–Lower Cretaceous Limestones From Bihor Mountains: Case Study Of Gârda Seacă-Hodobana Region, Romania, Valentin Turi, Emanoil Sasaran, Ioan I. Bucur Jan 2011

New Data On The Upper Jurassic–Lower Cretaceous Limestones From Bihor Mountains: Case Study Of Gârda Seacă-Hodobana Region, Romania, Valentin Turi, Emanoil Sasaran, Ioan I. Bucur

Studia UBB Geologia

This study refers to some problems regarding the lithological succession, facies and carbonate microfacies, and to biostratigraphic markers of the Upper Jurassic-Lower Cretaceous carbonates from Bihor Mountains. Three types of facies (external marginal facies, subtidal and peritidal facies) were separated for the Upper Jurassic, and two (coastal-peritidal and open shelf facies) for the Lower Cretaceous carbonates. The micropaleontological assemblages identified contain species that allow the separation of the two formations of different age: Labyrinthina mirabilis, Kurnubia palastiniensis, Neokilianina rahonensis, Clypeina sulcata (Kimmeridgian-Lower Tithonian) and Parakoskinolina? jourdanensis, Montseciella arabica, Palorbitolina lenticularis, Falsolikanella danilovae (Barremian – Lower Aptian). Field observations and data …