1311. |
1312. |
1313. |
1314. |
1315. Clinical features as a predictor of laparotomy findings in supradiaphragmatic stage I and II Hodgkin's diseaseMarjeta Vovk, Tatjana Šumi-Križnik, M... Jenko-Fidler, Gabrijela Petrič-Grabnar, M... Kremžar, Janez Novak, Mojca Senčar, Branko Zakotnik, A... Vodnik-Cerar, B... Jakšić, 1995, izvirni znanstveni članek Ključne besede: Hodgkinova bolezen, rak (medicina), klinična slika
Objavljeno v DiRROS: 15.01.2024; Ogledov: 247; Prenosov: 68
 Celotno besedilo (355,19 KB) |
1316. Pisma Johanna Jacoba Ferberja : geološki opisi Slovenije iz druge polovice 18. stoletjaMihael Brenčič, 2023, pregledni znanstveni članek Povzetek: Obravnavana sta prevoda pisem Johanna Jacoba Ferberja (1743–1790), švedskega geologa in mineraloga, ki je septembra 1771 potoval preko Slovenije. Prvo pismo, naslovljeno na Ignaza von Borna, je bilo objavljeno v knjigi »Pisma iz Italije o naravnih čudesih te dežele, ki so bila poslana naslovniku Ignacu plemenitemu Bornu«, ki je izšla leta 1773 v Pragi, drugo pismo, poslano Giovanniju Arduinu, pa najdemo v knjigi »Zbirka razprav s področja kemije, mineralogije, metalurgije in oriktografije«, ki je izšla leta 1775 v Benetkah. Obe pismi vsebujeta razsvetljenski znanstveni opis geologije dela območja današnje Slovenije, ki temelji na takrat veljavnih geoloških teorijah. V članku smo podali kratke življenjepise akterjev, prevoda obeh pisem ter njun komentar in interpretacijo.
Ključne besede: mineralogija, razsvetljenska geologija, regionalna geologija, zgodovina geologije, Giovanni Arduino, Ignaz von Born
Objavljeno v DiRROS: 15.01.2024; Ogledov: 341; Prenosov: 91
Celotno besedilo (2,19 MB) |
1317. Upper Triassic–to Lower Cretaceous Slovenian Basin successions in the northern margin of the Sava FoldsBenjamin Scherman, Boštjan Rožič, Ágnes Görög, Szilvia Kövér, László Fodor, 2023, izvirni znanstveni članek Povzetek: The evolution of the Slovenian Basin southern margin is currently interpreted based on the successions outcropping in the surroundings of Škofja Loka, on the Ponikve Plateau and in the foothills of the Julian Alps in western Slovenia, as well as from the valley of the Mirna River in south-eastern Slovenia. However, no extensive research on this paleogeographic unit has been carried out in the northern part of the Sava Folds region. Recent field observations permitted the recognition of Upper Triassic to lowermost Cretaceous successions of the Slovenian Basin, including the recently described Middle Jurassic Ponikve Breccia Member of the Tolmin Formation. Based on reambulation-type geological mapping, macroscopic facies observations supported by microfacies analysis and biostratigraphy, three stratigraphic columns were constructed showcasing Slovenian Basin formations on the northern flank of the Trojane Anticline (Sava Folds region). These newly described successions encompass Upper Triassic (Bača Dolomite Formation) and Jurassic–lowermost Cretaceous resedimented limestones and pelagic formations, while the attribution of the Pseudozilian Formation is complex. Based on facies characteristics these successions are similar to those preserved in the Podmelec Nappe (lowermost thrust unit of the Tolmin Nappe) in western Slovenia. The connection between the western and the eastern Slovenian Basin during the Late Triassic-Early Cretaceous interval could be thus recognised.
Ključne besede: Southern Alps, Sava Folds, Slovenian Basin, Jurassic, Ponikve Breccia, stratigraphy, foraminifera
Objavljeno v DiRROS: 15.01.2024; Ogledov: 336; Prenosov: 152
Celotno besedilo (27,89 MB) |
1318. Borers and epizoans on oyster shells from the upper Tortonian, Lower Chelif Basin, NW AlgeriaRachid Khalili, Linda Satour, Saci Mennad, 2023, izvirni znanstveni članek Povzetek: The three oyster lenses of the upper Tortonian of Djebel Touaka site which are described herein contain three species, Crassostrea gryphoides (Schlotheim), Ostrea lamellosa (Brocchi) and Hyotissa squarrosa (De Serre). The density of shell packing between the lenses is dissimilar. Most of the specimens are disarticulated and poorly fragmented; they exhibit a random distribution and orientation, without any distinct sorting. Bioerosion and encrustation are featured on both surfaces of left and right valves. The identified ichnogenera are Entobia (Bronn), Gastrochaenolites (Leymarie, 1842), Caulostrepsis (Clarke, 1908), Trypanites (Mägdefrau, 1932) and Maeandropolydora (Voigt, 1965). Encrusters are scared, represented by juvenile oysters/other bivalves, bryozoans and barnacles. The coexistence of borings on both sides of valves means that they probably occur not only while alive, but they keep happening after death. The oyster beds were deposited in a foreshore to shoreface environment, from the combined action of wave currents and sedimentation rate.
Ključne besede: Miocene, borings, encrustation, Entobia, Gastrochaenolites, Caulostrepsis, Trypanites, Maeandropolydora, foreshore, shoreface
Objavljeno v DiRROS: 15.01.2024; Ogledov: 234; Prenosov: 140
Celotno besedilo (20,32 MB) |
1319. Geological-genetic structure of Irpin city, the role of lithological factors during engineering-geological zoning and construction assessmentPavlo Zhyrnov, Iryna Solomakha, 2023, izvirni znanstveni članek Povzetek: The scheme of engineering-construction assessment created based on engineering-geological zoning of the city’s territory is desirable among additional graphic materials in the design of master plans projects as determined by building regulations. Engineering-geological zoning provides for different ranks’ selection of engineering-geological units (EG units), which have a particular range of common engineering-geological conditions that ultimately determine the construction sites’ affiliation to a specific suitability category. Geological-genetic structure of Irpin city of Kyiv region (Ukraine) is explored in this article. A variant of the creation of a large-scale engineering-geological map and corresponding geological-lithological sections by supporting boreholes in the borders of the city based on the engineering-geological survey conducted is presented. The obtained result allowed the selection of engineering geological zoning units – engineering geological districts by general conditions of geological development and subdistricts by engineering-geological complexes of Quaternary rocks’ thickness. The analysis of soils’ geomechanical properties (engineering-geological elements) lays the foundations for the selection of engineering-geological sites based on the comparison of this information with geomorphological, hydrogeological and geodynamic data. Accounting of geological-lithological factors in the preparation of the construction assessment scheme in the project of Irpin city’s master plan has become the ultimate result.
Ključne besede: engineering-geological zoning, engineering-geological units, geological-genetic structure, engineering-geological map, construction assessment
Objavljeno v DiRROS: 15.01.2024; Ogledov: 340; Prenosov: 158
Celotno besedilo (24,13 MB) |
1320. |
