BIOSTRATIGRAPHICAL SCHEME OF THE JURASSIC SEDIMENTS FROM PIENNINE ZONE OF UKRINIANE CARPATHIAN MTS

R.J. Leshchukh, G.I. Gotsanjuk

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: geomin@franko.lviv.ua

As a result of detailed study of Cephalopoda in Jurassic sediments from Piennine zone of the Ukrainian Carpathian Mts we have argued according to paleontology and proved using ammonites that all layers are present here. Also for the first time twelve hronozones of Jurassic system for this area we have picked out.

Key words:  Jurassic, biostratigraphy, layer, hronozone, Piennine zone, the Ukrainian Carpathian Mts, Cephalopoda, ammonites.

 

PROBLEMS OF THE GEOLOGICAL FORMATIONS SCIENCE

Ê.I. Sveshnikov

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: sveshn@franko.lviv.ua)

One of the most actual tasks in Geology is ordering of the data and development the science about the combinations of rocks steadily repeating in space and time (geological formations, elementary associations). Such combinations are fundamental divisions, homological to minerals and rocks. Problems of formations allocation among different rocks combinations and a question what classes (the big groups) of rocks combinations exist in the Nature are regarded in the article. Such combinations form lines with gradually varying properties, similar on principle to isomorphic lines of minerals are presentation by plutonia formations. The emerging of objects lines with gradually varying properties and some parallelism in changes of such properties in different lines are displays of the most general laws of structurization of the Nature. Isomorphic lines should be fixed as a basis for natural bodies classifications of all organization levels .

Key words: a rocks combination, geological formations, elementary associations, petrostructural class of the geological bodies, classification, an isomorphic line.

THE BEHAVIROUS ÑONSTRUCTING THE PHYSICS MODELS OF THE EARTH’S DEEP PROCESSES

V.V. Fourman, M.M. Khomyak, Yu.R. Datsjuk

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: geomin@franko.lviv.ua

Nonlinear effects in Geophysics is a new field of the Earth sciences developed and closely connected with nonlinear dynamics discordered deep layers in the Earth, synergetics, nonlinear geodynamics and thermodynamics. Various non-linear phenomena are observed in this field, including passive processes — propagation of seismic and electromagnetic waves and active processes manifesting in geodynamical characteristics, interaction of fields of different physical nature in the deep layers of the Earth. These interactions do concern the Earth spheres — lithosphere, mantle, core, atmosphere and hydrosphere, and space as well, reflect and influence the course of geological evolution of the planet in the Universe.

Key words: physic of the Earth, modelling, deep processes.

 

CRITERIONS OF THE GOLD-BEARING TERRITORIES FORECAST VALUATION

(theoretical and methodological principles)

Liakhov Yr.V., Pavlun` M.M., Pakhniushchyi Y.O., Lun`ov G.O.

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: geomin@franko.lviv.ua

Theoretical and methodological principles of the elaboration and realization  of the criterions of gold-bearing  territories forå casting vàluation has been exràmined.

Key words: criterions, forecast, gold-bearing  formations, thermobarogeochemistry.

 

FACTOLOGY SPATIAL MODELLING FLUID PALEOFLOODS  BEHIND THE DATA

(on an example gold-ore deposits of Northern Buriatiya)

I.V. Popivnyak

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: geomin@franko.lviv.ua

Results of spatial factology modelling of the endogenie the fluid paleoflows  on many gold-ore deposits are presented. On the base of data of thermobarochemistry the features of morphology and morphometry fluid paleoflows have been distingiushed. Inconvertibility and asymmetric orientation of migration of mineralgenesis fluids is proved, to feature of their concentrated or absent-minded functioning in the field of localization of ores. It is shown, that spatial variability of thermobarochemistry characteristics (Ð, Ò, V etc.) of the inclusions fluids received by results of research displays features of dynamics (changes) and physical and chemical conditions at which once migrated mineralgenesis fluids. Results of the research testify, that the raised(increased) concentration of gold (ore columns) always are located in borders fluid paleofloods.

Key words: thermobarochemistry, fluid paleoflows, modelling, inclusions fluids, gold-ore deposits.

 

MINERALOGICAL ZONATION GOLD MINERALIZATION OF THE RAKHIV ORE REGION

S.I. Tsikhon`

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: tsikhon_s@ukr.net

The peculiarities of the minerals and mineral associations distribution within Rakhiv ore region have been investigated. High-temperature mineral associations as was revealed are wide-spread mainly in the central and medial blocks of the Sauliakh radial-circular structure while middle-temperature (productive) with, a gold – in the medial and peripheral ones and late (low-temperature) – mainly in the peripheral blooks .

Key words: Rakhiv ore region, minerals, mineral associations, mineral forming, radial-circular structures, zonation, gold, ore manifestation.

 

TECTONOGENESIS OF  THE UKRAINIAN SHIELD SAVRANO-SYNYTSIVSKA AREA (MIDDL POBUZZIA)

O.B. Bobrov, V.M. Shevchuk*, I.M. Turchynovskiy*, O.V. Shvayevskiy*

Ukrainian State Geological Research Institute, Àvtozavodska St. 78, UA–04114 Êyiv

 e-mail:à_bobrov@inbox.ru

*Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA–79005 Lviv

e-mail: geomin@franko.lviv.ua

Tectonic structure, formation filling and shaping sequence of the folded formations of the  Savrano-Sinitsivska Ukrainian Shield area are considered. Three main stages of the folding and structural rebuilding of the area has been determined. Some special spatial-temporal interrelations of the gold mineralization forming as well as folding has been revealed.

Key words: Charnockite-granulitic complex, structural-geometric analysis, fold, axial line.

 

THERMOELECTRICE PROPERTIES OF PYRITE OF LADISLAV ORE MANIFESTATION (RAKHIV REGION)

L.M. Hopko, V.P. Marusyak, T.P. Oliynyk, I.V. Popivnyak, S.I. Tsikhon

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: geomin@franko.lviv.ua

Thermoelectricte properties of pyrite of Ladislav ore manifestation (Rakhiv ore region) have been investigated.

Key words: typomorphism of minerals, thermoelectric, sulphyides, gold, pyrite.

 

PHYSICAL-CHEMICAL ORE-FORMING CONDITIONS IN THE BAROON-HOLBINS’KE GOLD DEPOSIT AND IN THE LYPNYAZHKA ORE FIELD

(comparative character)

T.Î. Pavliuk

Ivan Franko National University of Lviv, Hrushevskyi st. 4, UA – 79005 Lviv

e-mail: geomin@franko.lviv.ua

Similarity and distinction of the physical-chemical forming conditions in Baroon-Holbynske gold deposit (East Sayan) and in Lypnyazhka ore field (the Ukranian Shield) have been considered by the methods of thermobarogeochemical investigations.

Key words: gold-bearing deposit, thermobarogeochemistry, fluid regime, physical-chemical forming conditions.

COAL OF THE L'VIV-VOLYNS’K COAL FIELD

Yu.S. Makovskyi

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: geomin@franko.lviv.ua

The data of the different researches about paleogeography and tectonic position of the basin in Carboniferous period are compared. The complex of factors by which accumulation of coal formation of the Lviv – Volyns’k basin was completed during the Carboniferous period is examined. The geographical position, character of variability facies ash values and accumulation of deposits in pool and features of a geodynamic mode of territory are analyzed.

Key words:  coal formation, Lviv-Volyns’k Carboniferous basin, processes of accumulation of the vegetative rests, paleogeography, climate, tectonic zonation.

 

ULTRAPOTASSIC RHYOLITES OF ACTIVIZED REGIONS

S.S. Kryzhevych, V.B. Stepanov

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: geomin@franko.lviv.ua

Metallogenic significance of the ultrapotassic rhyolites for different regions is shown. This rocks group for the first time had been distinguished by authors on the Northen Caucasus. Its geological situation character, rhyolites petro-geochemical peculiarities and metallogenic role are presented. Presence of the ultrapotassic rhyolites in gold-bearing Transcarpathian region is assumed.

Key words: ultrapotassic rhyolites, metallogenic significance.

 

EARLY CRETACEOUS STAGE OF NAPPE FORMING OF THE UKRAINIAN CARPATHIAN

L.N. Khomyak

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: zaggeo@franko.lviv.ua

In Early Cretaceous time an extension and destruction of the crust in the Carpathian region was changed to contraction conditions. The separate massifs in the Inner Carpathian come into collision with the foundation of the flysch geosyncline, that leaded to forming napped structures of Early Cretaceous generation. In the work the process of structural and sediment transforming in the boundaries of the Ukrainian Carpathian is analyzed, which caused by pushing of the flysch basement under Marmarosh massif in Barremian and Aptian time.

Key words: Carpathian region, napped structures, Early Cretaceous time, Marmarosh massif, flysch basement.

 

STRUCTURAL-TEXTURE PECULIARITIES OF THE COPPER-BEARING FLYSCH FROM UKRAINIAN CARPATHIAN SCYBOV ZONE

V.O. Khmelivsky,  Î.V. Kostyuk,  ².P. Mydruk

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: geomin@franko.lviv.ua

The inportance of the Ukrainian Carpathian flysch deposit litholostructure, bedding and texture peculiarities of the Yaremtcha horizon had been described. Texture peculiarities of the Yaremcha horizon deposits as was ascertained don`t differ esscutially from Cretaceous and Paleogene deposits.

Key words:  Yaremcha horizon, skew lamination, ³mpressions bound with habitability organizm, dyke.

 

CHEMISTRY OF MINE WATERS CHERVONOGRAD OF MINING AREA, AS ONE OF FACTORS OF NEGATIVE INFLUENCE ON THE GEOLOGICAL ENVIRONMENT

Yu.V. Yarosh, V.V. Kharkevich*

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: admingeo@franko.lviv.ua

*Dð. “Zahidukrgeologia”, ðl. Mitskevich 8, UA – 79000 Lviv

Chemistry mine waters Chervonograd mining area is investigated. Contents of mine waters cations (Na++K+, Ca++, Mg++  ), anions  (Cl-, SO4-- ),  microelements (J, Br, F, Ba, Mn, Cr, Sr, Ti) general hardness were analized. It is found out the contents by results of researches, that average contents of chemical elements in system “mine – the sediment bow” decreases.

Redutiction contents of chemical elements is caused by recucling of deposits and dissolution of waters by an atmospheric precipitation.

Distribution of element contents  in mines and sediment bowls is represents as a graphic material. Negative effect of mine waters on the geological environment is shown. Mine waters pollute ground, underground and superficial waters. Possible variants of  land reclamation  and reduction of negative effect  of these waters on the environment are given.

Key words: Mine waters, the sediment bow (pond – store), upper level concentration (ulc),  the average content of  element, ecological effect, the geological environment.

 

DISTRIBUTION OF CHEMICAL ELEMENTS CONTENTS IN ROCKS WASTE DUMPS IN CHERVONOGRAD MINING AREA

I. B. Knysh,  V.V. Kharkevych*

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: admingeo@franko.lviv.ua

*DP “Zahidukrgeologia”, sq. Mitskevich, 8, 79000 Lviv. Ua.

Vertical and plane distribution of the chemical element contents in rocks of waste dumps of mines in Chervonograd mining area is investigated. The short analytical review of chemical element content in coal, and coal formation, and their ecological effect on geological environment is given. The analysis of chemical elements distribution in rocks of waste dumps is submitted, and vertical and plane changes in contents  of characteristic chemical elements are presented. The contents of elements in rocks waste dumps are found out to be above the average content elements in coal formation. Waste dumps are considered to be “concentrating factories” for chemical elements. Distribution of content of elements on vertical and plane is illustrated  by graphic material. The stated results enable to raise the question about waste heaps as new “technogenous” deposits of minerals and to estimate their ecological effect on the environment. 

Key words: waste dumps, mine, plane and vertical distribution, the content of a chemical element, clark, GDK.

 

DOCTOR of  SCIENCES (Geology), PROFESSOR VOLODYMYR VASYLIOVYCH KOLODIY  SCIENTIST AND PATRIOT (to 70  from birthday )

R.J. Leshchukh, V.V. Karabyn

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA79005 Lviv

å-mail: admingeo@franko.lviv.ua

Biography of famous Ukrainian scientist, Doctor of geological-mineralogical sciences, Head of Ukrainian national committee of Carpathian-Balkan geologic association, Head of Geologic commission of Shevchenko Scientific Society, Professor of Ecological and Engineering Geology and Hydrogeology  Volodymyr Vasyliovych Kolodiy is presented. The analysis of the most important scientific publications is made.

Key words: Volodymyr Kolodiy, oil-accumulation, oil-and-gas-bearing field, underground waters, Hydrogeology,  History of a science.

 

GEORGIJ BOJKO – THE SCIENTIST-OILMAN

P.M. Bilonizhka, R.J. Leshchukh, V.O. Fedyshyn

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: geomin@franko.lviv.ua

Scientific activity of the wellknown Ukrainian scientist in the field of Oil-and-Gas Geology and Geochemistry, Mineralogy of organic substances and the researcher of history of geological science in Galitsia Georgij Bojko is analysed.

Key words: Georgij Bojko, Mineralogy of ozokerite, Oil-and-Gas Geology, origin of petroleum, history of science.

FROM HISTORY OF GEOPHYSICAL RESEARCH IN IVAN FRANKO LVIV NATIONAL UNIVERSITY

R. Vovchenko, V. Fourman, A. Polubichko

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: geomin@franko.lviv.ua

History of geophysical researches and science has been analyzed as well as teaching of science about Earth in Lviv university for the past century. Life path and scientific activity of famous scientists in those branches of science have been enlightened among of Prof. Henrich Artztovskij, founder of Ukrainian Geophysics, Ac. Volodymyr Selskij and Ac. Serafym Subbotin.

Keywords: Physics of the Earth, geophysical researches, G. Artztovskij, V.O. Selskij, S.I. Subbotin, Ivan Franko Lviv National University.

 

177VASYL SHEREMETA – THE STRATIGRAPHER, THE PALEONTOLOGIST, THE PEDAGOGUE

P.M. Bilonizhka, R.J. Leshchuêh

Ivan Franko National University of Lviv, Hrushevskyi St. 4, UA – 79005 Lviv

e-mail: eñogeo@franko.lviv.ua

The paper is devoted to memory of the wellknown scientist of reseacher  of Paleogene, Neogene deposits and ostrakods of  Ukraine Assistant  Professor  Vasyl’ Sheremeta.

Key words: Vasyl’ Sheremeta, stratigraphy, ostrakods, Paleogene, Neogen of Ukraine, paleogeography, pedagogical and public activity.