Authors:S. Alcay, C. Inal, C. Yigit, and M. Yetkin
Nowadays, GPS is the best positioning system with its constellation, but number of GLONASS satellites increased to the required number, with launched new ones, for positioning. With recent revitalization of GLONASS, a great number of high precision GLONASS and GPS/GLONASS receivers have been produced. In this paper, baselines of two networks have been analyzed in order to assess the usability of GLONASS on global positioning. In both networks, repeatabilities of results were investigated by using GPS, GLONASS and GPS/GLONASS data. Results revealed that repeatabilities of all baselines by using GLONASS observations are not consistent when compared to the GPS and GPS/GLONASS.
A single tooth from the locality of Üröm-hegy (Hungary) was designated as the holotype specimen of “Archidiskodon meridionalis ürömensis” by Vörös (1979). The observed morphology of the tooth, with a minimum of 15 molar plates (most likely 17) led to the conclusion that this specimen belongs to Mammuthus trogontherii rather than a subspecies of M. meridionalis. On the basis of rodent biostratigraphy a date in the region of MIS 19-17 seems likely (i.e. c. 0.8 Ma — c. 0.7 Ma). Taking into account the meridionalis-like enamel thickness (3.1 to 3.4 mm, mean 3.2 mm) as well as the intermediate or slightly advanced relative crown height (1.65) and lamellar frequency (6), the specimen shows mosaic morphology, which fits well in the framework of the contemporaneous European mammoth-bearing localities (e.g. Voigtstedt). Taking all the evidence together it seems that this molar is not only a misinterpreted specimen, but a representative of a very important period of mammoth evolution in Eurasia, when M. meridionalis and M. trogontherii occurred together in Europe and when the genetic mixing between the adjacent populations resulted in a hybrid zone, which was responsible for mosaic or intermediate individuals, such as the holotype of “Archidiskodon meridionalis ürömensis”.
mediterranean basins: Tertiary extension within the Alpine orogene , Vol. 156 . Geological Society , London , Special Publication , pp. 215 – 250 . Vass , I. , M Tóth , T. , Szanyi , J. , and Kovács , B. ( 2018 ). Hybrid numerical modelling of
Authors:Elemér Pál-Molnár, Luca Kiri, Réka Lukács, István Dunkl, Anikó Batki, Máté Szemerédi, Enikő Eszter Almási, Edina Sogrik, and Szabolcs Harangi
environment (at 230 Ma); (2) 215 Ma ago the subsolidus gabbroic-dioritic magma intruded into the crust and interacted with the crustal syenitic melt. Hybrid rocks were formed as a consequence of magma mixing and mingling; (3) parental melt of nepheline syenite