P. 3-7
SOME EXTREMELY PREDICTIVE FEATURES OF ACADEMICIAN V.I. VERNADSKY’S RESEARCHES
(to the 150th anniversary of his birth)
N. Pavlun’
Ivan Franko National University of Lviv,
geological faculty, department of geology of minerals,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
e-mail: zaggeol@franko.lviv.ua
The predictive power of some ideas of eminent scientist V.I. Vernadsky is briefly described.
Key words: V.I. Vernadsky, biosphere, biogeochemistry, mineralogy, radiogeology, geological ages of life.
P. 8-17
VОLОDYMYR VERNADSKYJ – THE FOUNDER OF UKRAINIAN ACADEMY OF SCIENCES
P. Bilonizhka
Ivan Franko National University of Lviv,
geological faculty, department of geology of minerals,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
e-mail: mineral@franko.lviv.ua
The role of Vernadskyj in establishing of Ukrainian Academy of Sciences, his contribution to the scientific and organizational work, search for scientific personnel and development of the world dimension of the Academy are covered. The history and UAS in the first decade of its existence is briefly described.
Key words: Ukrainian Academy of Sciences, Vоlоdymyr Vernadskyj, scientific and organizational activities, the Charter of UAS, the history of UAS.
P. 18-32
THE MODELING OF GEODYNAMICAL AND ENERGY TRANSFORMATIONS
IN ACTIVE ZONES OF THE EARTH СRUST AND MANTLE
V. Fourman
Ivan Franko National University of Lviv,
geological faculty, department of physics of the Earth,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
e-mail: fourman@franko.lviv.ua
The main issues of tectonics are considered and review of the main problematic questions which form the ways of investigation of the physical image of structures as well as of processes and interactions in the deep shells of our planet is made. Main forces acting within subduction zone are slow convective currents in mantle and slab detachment. Depended on tectonic deformation measurements and dates about moving the causes of tectonic activity of the platform crust within different deeps are determined. The effectiveness of the complexity of different geophysical data for authenticity of geodynamic situations with examples from Alpine mountain chains is shown.
Key words: Geodynamics, Thermodynamics, Tectonics, structure of the Earth, modelling, deep processes, physical modelling.
P. 33-39
DYNAMICS OF POSTSEISMIC TECTONIC DEFORMATIONS
D. Malyckiy, S. Kravets
Сarpathian branch of Subbotin Institute of geophysics,
Naukova Street, 3-b, 79060, Lviv, Ukraine,
e-mail: adm@cb-igph.lviv.ua
The results of deformographycal measurements carried out on Trans Carpathian seismic zone are analyzed. The aim of research is to study the modern tectonic processes caused by a postseismic activity.
Key words: geodynamics, seismology, deformations, monitoring of dangerous processes.
P. 40-45
THE PROSPECTS FOR RESEARCHING THE PROTO BASEPLATE MARGIN IN THE EARTH’S CRUST
OF THE WESTERN REGION OF UKRAINE
Kh. Zayats
Lviv Department of UkrSGPI,
Pasichna Street, 38 a, 79038, Lviv, Ukraine,
e-mail: mych@gmx.net
According to the data of seismic studies conducted in the South of the Western region of Ukraine, a new margin is found in the granitic stratum of the Earth’s crust and maned the proto baseplate. The characteristics of the margin allow to forecast the geodynamic development of the Earth’s minerals which influenced the structural composition and conditions of oil and gas conductivity of the sedimentary cover.
Key words: seismic survey, crust, protofundament.
P. 46-68
THE PROBLEM OF LVIV REGION WATER RESOURCES PROTECTION
V. Kharkevych1, Y. Misiura2
1Ivan Franko National University of Lviv,
geological faculty, department of ecological and engineering geology and hydrogeology,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
e-mail: admingeo@franko.lviv.ua
2Lviv Department of UkrSGPI, Pasichna Street, 38 a, 79038, Lviv, Ukraine,
e-mail: lv_ukrdgri@polynet.lviv.ua
Three types of feed areas of underwater artesian deposits are described: area of feed, located in higher in relief part of locality; a feed which runs through the rivers on crack areas; a feed which is in deep breaks. The essence of water protection from contamination is described.
Key words: area of feed, contamination, water, protection, water horizon.
P. 69-80
ASSESSMENT OF KALUSH AND HOLYNSKA POTASSIUM SALT
DEPOSITS AND TAILINGS INFLUENCE ON
GEOCHEMICAL CHARACTERISTICS OF RIVER WATER
I. Kytsmur, V. Dyakiv
Ivan Franko National University of Lviv,
geological faculty, department of ecological and engineering geology and hydrogeology,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
e-mail: kytsmur89@gmail.com, dyakivw@yahoo.com
The zone of Kalush and Holynska deposits of potassium salts, Kalush in particular, villages Kropuvnuk and Sivka-Kaluska, were declared as ecological disaster zone in 2010. One of the most actual problem of the area is the erosion of precipitation saltbearing heap overflow tailings and dissemination areola as salinity groundwater and surface water, as well as the risk of a essential deterioration in water quality in the city's water intake. To assess the actual state of river water in the studied area during low-flow held their checking detailed geochemical sources of pollution to the peripheral areas. Two mechanisms of demineralization of river water – gravitational infiltration of water with a salinity of more than 5,0–10,0 g/l runoff and dilution water with distance from the source of pollution due to increased water content of the channel flow have been determined.
Key words: Kalush-Holyn deposit of potash salts, salt dump, tailings, infiltration, rivers Sivka, Mlynivka, Kropyvnyk, river water geochemistry, demineralization, dilution.
P. 81-93
USING OF MODEL-OBJECTS OF DIAMOND DEPOSITS
DURING PROGNOSIS-EXPLORATION ACTIVITY IN ISSUES OF MODERN DIAMOND GEOLOGY
V. Guliy, I. Poberezhska
Ivan Franko National University of Lviv,
geological faculty, department of petrgraphy,
Hrushevsky str., 4, 79005, Lviv, Ukraine,
e-mail: vgul@ukr.net, irina_pober@ukr.net
Peculiarities of prognosis and perspective recourses calculation of diamond, which are based on using the model objects with industrial scale of concentrations or under mining, are given in present article. To create model characteristic for diamond deposits, diamond-bearing rocks of the French Guiana have been used as example. Typical features of geological-structural position as well as petrography and mineral composition authors compared with potential diamond- bearing rocks of greenstone structures of the Ukrainian Shield. Results of such comparison were analyzed to determine perspective sectors by different petrochemical diagrams. They showed some similarities between model objects and the separate sectors of greenstone structures of Ukrainian Bed after a number of chemical components and indicators of comatiites.
Key words: diamond, industrial deposits, prognosis and exploration, model-objects, comatiites, Ukrainian Bed, French Guiana.
P. 94-103
GEOSOLITON CONCEPTION OF HYDROCARBON ORIGIN
UNDER GEOLOGICAL CONDITIONS OF UKRAINE
G. Lepigov1, V. Guliy2, I. Poberezhs’ka2, A. Loktev3
1Ukrainian State Geological Research Institute,
Avtozavods’ka Street, 78, 04114, Kyiv, Ukraine,
2Ivan Franko National University of Lviv,
geological faculty, department of petrography,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
e-mail: vgul@ukr.net, irina_pober@ukr.net
3Geological-Thematycal Center UkrNDIgaz, Ugers’ke, Ukraine,
е-mail: vgul@ukr.net
Role of geosoliton conception in abiogenic theory of hydrocarbon genesis is discussed in this article. The background of the conception is an idea about permanent degassing of the Earth and moving of the materials, which are rich in substation of the Earth crust and mantle, in form of flows-solitons. Soliton is a special kind of substation between solid rocks and radiation (particle and photon). In subvertical zones of destruction (SZD) in upper mantle and earth crust these flows form a new structural formations – geosoliton chimney rich in fluids due to the materials from surrounding rocks and which are characterized by anomaly of high pressure and temperature. Geosoliton chimneys contain high debit concentration of hydrocarbons, which we can see in number of oil and gas fields in the Western Siberia, Sakhalin, Brunei, etc. The geosoliton conception which is obtained as a part of the theory of abiogenic genesis of hydrocarbons, can be a serious positive movement in practice of exploration of gas and oil fields in Ukraine.
Key words: abiogenic genesis of hydrocarbons, degassing of the Earth, geosoliton, subvertical zone of destruction, resources of hydrocarbons, oil and gas fields, gas column.
P. 104-115
SOME FEATURES OF VULCANITES CHEMISM OF
TROSTYANETSKY MESOZOIC COMPLEX (UKRAINIAN CARPATHIANS)
L. Gеnеrаlоvа, V. Pаshchеnко, V. Stеpаnоv
Ivan Franko National University of Lviv,
geological faculty, department of general and regional geology,
department of petrography,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
e-mail: vl_pasha@mail.ru
Some peculiarities of the vulkanites chemistry of Mesozoic Trostyanets complex are considered. It is concluded that the volcanic rocks combine mixed petrochemical characteristics. Some characteristics are peculiar to the top of ophiolite association, others correspond to the magmatism of shear conditions.
Key words: Ukrainian Carpathians, Trostyanets complex, vulkanites, basalts.
P. 116-121
ON THE FORMATION OF GRANULAR OF COLLECTORS
OIL AND GAS DEPOSITS
R. Smishko
Ivan Franko National University of Lviv,
geological faculty, department of general and regional geology,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
e-mail: zaggtjk@franko.lvsv.ua
Organic substance of biogenic origin takes an active part in the forming of sedimentary rocks. Interaction of mineral (inorganic) part of rock with organic matter is obvious. Activation of fluid’s reaction ability during tectonic movements (folding) is depended on their additional saturation by organic matter during migration that leads to recrystalization of primary rocks and development of secondary porosity.
Key words: granular collector fluid, organic matter, silica , quartz, hydrocarbons.
P. 122-130
PALEOSTRESS FIELDS FEATURES AND TECTONIC JOINTS IN
THE CHORNA TYSA RIVER VALLEY (PORKULETS AND DUKLA NAPPES)
S. Kril1, I. Bubniak2, Yu. Vikhot2, S. Tsikhon1
Ivan Franko National University of Lviv,
geological faculty, 1department of geology of minerals,
2department of physics of the Earth,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
е-mail: solia_kr@ukr.net, ibubniak@yahoo.com, yuvik@ukr.net,
tsikhon_s@ukr.net
Results of the detailed new tectonophysical and structural researches in the Porkulets and Duklya nappes of the southeastern part of the Ukrainian Outer Carpathians were interpreted. Field investigations were carried out in 2010-2011 in the Chorna Tysa river valley, from Kvasy to Bilyn villages (Rakhiv region, Transcarpathian). More than 400 orientations of tectonic joints, 30 slickensides in outcrops and in the sides of the roads in 8 points of observation were measured and studied in detail. Reconstructed by complex using of structural-paragenetic and kinematic methods sequence of paleostress fields with orientations of the principal axes (σ1, σ2, σ3) indicates changes of the deformation regimes during Cenozoic time. Identified by joints and slickensides strike-slip deformation regime in post folding-faulting time is possibly connected with the Rakhiv-Tysa fault zone formation. Rose-diagram of the 140 joints filled with calcite orientation was created. Calcite was formed within the systems of different age joints.
Key words: Ukrainian Carpathians, Porkulets and Duklya nappes, Rakhiv-Tysa fault zone, paleostress fields, joint, slickenside.
P. 131-137
TOWARDS THE CORRELATION TECHNIQUE OF DISCONNECTED
GEOLOGICAL SECTION OF THE FERRUGINOUS SILICEOUSSHALE
STRATUM IN THE KRYVYJ RIH BASIN
S. Radovanov
State Survey of Geology and Subsurface of Ukraine,
Eugène Pоttier Street, 16, 03057, Kyiv, Ukraine,
e-mail: sekretar@geomail.kiev.ua
Methodological questions of correlation between separated geological sections of ferruginous siliceous-schist strata in Kryvyj Rig iron-ore basin are discussed on the base of geological-formational analysis.
Key words: correlation, paragenesis, ferruginous siliceous-shale stratum, Kryvyj Rih Basin.
P. 138-145
GEOCHEMICAL CHARACTERISTICS OF MINE WATERS OF
CHERVONOGRAD MINING-INDUSTRIAL DISTRICT
S. Voitovych
Ivan Franko National University of Lviv,
geological faculty, department of petrgraphy,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
e-mail: starostasvetik@mail.ru
Based on systematic analysis of component composition of mine water Chervonograd mining - industrial area distribution pattern in these essential components is defined. Determined prevailing water classes is: a) Cl-> SO4 2+> HCO3- b) Na+> Ca2+>Mg2+. Based on factor analysis the fact of mixing mineralized coal and fresh waters senon water-bearing complexes is established.
Key words: mine water, correlation analysis, regression analysis, factor analysis, Chervonograd mining-industrial district.
P. 146-147
NEW RUSSIAN-UKRAINIAN GEOLOGICAL DICTIONARY
P. Bilonizhka, M. Pavlun’
P. 148-151
THE GEOLOGICAL RESEARCHES HISTORY AT LVIV UNIVERSITY (the 50th anniversary edition of the Bulletin)
M. Pavlun’, P. Bilonizhka
P. 152-176
HISTORY OF VIEWS ON GEOLOGICAL STRUCTURE OF THE CARPATHIANS
P. Lozynjak
Lviv branch UkrDGRI,
Pasichna Street, 38a, 79038, Lviv, Ukraine
In this work the different concepts of the geological structure of the Carpathian fold structures and shows the development of the mining industries in the region. Highlights also the issue of the age and origin of the Carpathian sandstone formation and rocky out crops of Mesozoic limestones (klipens) as Southern (Bratislava–Novoselytsia–Maramorosh) and northern (Krasnoputnenskoyi) bands.
Key words: Carpathian fold construction, mining industries, Carpathian sandstone, klipens.
P. 177-179
DR. ROMAN YOSYPOVYCH LESCHUKH – 70th ANNIVERSARY
J. Krupski, J. Naumko, M. Pavlun, V. Fedyshyn
P. 180-185
60th ANNIVERSARY LARYSA VOLODYMYRIVNA GENERALOVA
A. Sivoronov, M. Pavlun, P. Bilonizhka
P. 186-188
FOURTH ANNUAL NATIONAL CONFERENCE “CURRENT ISSUES IN UKRAINE GEOLOGICAL RESEARCH”
G. Hotsanyuk
P. 189-190
STUDENTS THAT WERE GRADUATED FROM GEOLOGY DEPARTMENT
IVAN FRANKO NATIONAL UNIVERSITY OF L’VIV AT 2013 YEAR
P. Bilonizhka, O. Polubichko