DMYTRO PETROVYCH REZVOY – THE GEOLOGIST AND THE SCIENTIST
(regarding the 100th anniversary of birthday)
А. Sivoronov, L. Generalova
Ivan Franko National University of Lviv,
geological faculty, department of general and regional geology,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
e-mail: zaggeol@franko.lviv.ua

The contribution of professor D.P. Rezvoy– the outstanding geologist – to the develolopment of modern geotectonic is briefly described. It is marked that all his works were pioneer to Central Asia and Ukraine
Key words: geosynclinal system, deep fault, tectonic zoning, formation, Central Asia.

HISTORY OF THE THERMOBAROGEOCHEMISTRY
INVESTIGATION ON THE GEOLOGICAL DEPARTMENT:
FORMATION STAGE AND THEORETICAL-APPLIED CONSEQUENCE
M. Pavlun’
Ivan Franko National University of Lviv,
geological faculty, department of geology of minerals,
Hrushevskij Street, 4, 79005, Lviv, Ukraine
e-mail: zaggeol@franko.lviv.ua

Chronological and logic stages of the formation and development of the thermobarogeochemical investigation of the fluid inclusions in minerals are considered.
Key words: thermobarogeoсhemistry, fluid includings, post-magmatic structures, gydrotermal solutions.

METALLOGENY OF DONBAS AND CARPATHIANS
IN THE WORKS OF YEVHEN LAZARENKO
O. Matkovskij
Ivan Franko National University of Lviv,
geological faculty, department of mineralogy,
Hrushevskij Street, 4, 79005, Lviv, Ukraine,
e-mail: mineral@franko.lviv.ua

The works, devoted to different aspects of Carpathians and Donbas metallogeny, have a great significance in many-sided scientific legacy of Ye. Lazarenko. The maiden attempts of development of Donbas metallogeny as well as the creation of the first model of metallogenic map on the scale 1:1 000 000 and legend to it belong to the scientist. Metallogenic map of Carpathians on the scale 1:1 000 000 has been published under the editorship of Ye. Lazarenko.
Key words: Ye. Lazarenko, metallogeny, metallogenic map, Donbas, Carpathians.

GEOTECTONIC NATURE OF GREENSTONE BELTS
OF THE LOWER PRECAMBRIAN
А. Sivoronov
Ivan Franko National University of Lviv,
geological faculty, department of general and regional geology,
Hrushevskij Street, 4, 79005, Lviv, Ukraine
e-mail: zaggeol@franko.lviv.ua

In order to understand the tectonic history of granite-greenstone areas important is the "pre-greenstone stage" is important, during which heterogeneous basement of greenstone belts was formed and consists of two Lower Cambrian complexes (charnokitegranulitic and plagiogranitoid-amphibolic). They differ by metamorphism, composition of supercrust and granitoid formations, and tectonic structure. The development of greenstone belts is divided into 4 stages by the nature of formation sets and their position in evolution of granitoid magmatism. Substance feature of the first pre-greenstone (pre-rift) stage is fairly specific aplite-pegmatoid formation that formed by anatexis of greenstone belts. In the second (rift) stage in the geodynamic conditions of tension of crust began the formation of greenstone deeps. The third stage is diapir stage of develoment of greenstone belts. It is indicated by a new surge of thermal activity of these structures and risen of large masses of tonalite magma and processes of granitoid diapirism. In the fourth stage of stabilization of the consolidation of greenstone deeps and rooting very large intrusive bodies in two feldspathic certainly porphyraceous granites.
Key words: greenstone belts, greenstone deeps, granitoid diapirism, tonalites, charnokite-granulitic and plagiogranitoid -amphibolic complexes.

MODELLING OF THERMOMECHANICAL PROCESSES
IN THE AREAS OF ACTIVE INTEROPERABILITY
OF CURST AND MANTLE OF THE EARTH
V. Fourman
Ivan Franko National University of Lviv,
geological faculty, department of physics of the Earth,
Hrushevskij Street, 4, 79005, Lviv, Ukraine,
e-mail: fourman@franko.lviv.ua

The model has been developed and analytical solutions of identifying deformations in the active areas crust and the mantle of the Earth were found, deformations which were created by natural effective anomalous densityin the gravitational field of the Earth. On the basis of numerous modelling of the developed convection in conditions of a mantle of the Earth there is a possibility to investigate an interoperability of mantle convection with lithosphere and to restore the distribution of temperature in the top part of lithosphere.
Key words: mantle convection, termomechanical processes, crust, astenosphere.

MINERAGENETIC FEATURES OF WESTERN SLOPE
OF THE UKRAINIAN SHIELD IN FLUIDIZATE-EXPLOSIVE
ASPECT (DNISTER REGION)
G. Yatsenko, O. Buchkovska
Ivan Franko National University of Lviv,
geological faculty, department of geology of minerals,
Hrushevskij Street, 4, 79005, Lviv, Ukraine,
e-mail: Yatsenko1941@list.ru

It is shown that geological-structural features of western slope of the Ukrainian shield are propitious to localization of ore-bearing structures of fluidizate-explosive type. They contain diamonds, gold, polymetallic ores, bauxites, fluorite etc. Metasomatic, hydrothermal and sedimentary processes are involved in ore formation. Expedience of continuation of actions in this direction is explained.
Key words: Ukrainian shield, western slope, fluidizates, ore-bearing structures, deposits, mineragenesis.

COMPOSITION, QUALITY, GENESIS OF COAL, STRATIFICATION,
CORRELATION, AND CONDITIONS OF THE COAL–BED h7 CUT
ORMING ON THE TERRITORY OF DONETSK–MAKIIVSK AREA OF DONBASS
V. Uziuk¹, O. Shvartsman^2
1Ivan Franko National University of Lviv,
geological faculty, department of historical geology and paleontology,
Hrushevskij Street, 4, 79005, Lviv, Ukraine,
e-mail: coalgeol@franko.lviv.ua
²Artemivs’ka GRE DGP “Donbasgeologia”,
Sуbirceva Street, 17, 84500, Artemivsk, Ukraine

The changes of the coal-bed geological structure in the mine workings of the mines and seven monolithic cuts are described, selected in the coal-faces of the drifts; macroscopic the features of coal and their changes from the base to the top of every cut: maceral, chemical the composition, technological the properties, brand the belonging and the coal metamorphism of sectional samples, that from complete coal-bed the cuts; the peculiarities of microlithotypic the composition change and the coal-forming plants´ associations from the base to the top of the coal-bed . The correlative coal characteristics of every cut are defined and described. The detailed stratification and the coal-bed cut correlation are carried out and described, as well as their synonymy is developed. The directions of the rational coal use in the national economy are defined.
Key words: coal-bed, monolithic cut, drift, coal, maceral, microlithotypic, chemical composition, technological properties, brand, metamorphism group.

GEOGYNAMIC RECONSTRUCTIONS
OF THE LOWER-MEDDLE PALAEOZOIC SERESUJSK
VOLCANOGENIC-SEDIMENTARY STRUCTURAL-FORMATIONAL
COMPLEX OF THE NORTH-EASTERN FERGHANA (TIEN SHAN)
L. Generalova
Ivan Franko National University of Lviv,
geological faculty, department of general and regional geology,
Hrushevskij Street, 4, 79005, Lviv, Ukraine,
e-mail: zaggeol@franko.lviv.ua

Seresujsk volcanogenic-sedimental structural-formation of the Lower–Middle Paleozoic complex of the Nort-Eastern Ferghana includes three siliceous formations: seresujsk siliceous-plate formation of the Silurian, ajrutashsk limestone-volcanic-siliceous formation of Middle Devonian, karacolsk siliceous-limestone. formation of the Lower Carbon. Substance, textural and petrochemical peculiarities of the rocks of formations were investigated. It is possible to conclude that this formation appeared on the oceanic crust, which eventually were transformating to the crust of passage type. Creation of these formations we can compare with geodynamical conditions of the abyssal plain and continental foot.
Key words: North-Eastern Ferghana,Tien-Shant, volcanic-sedimentary complex, structural-formational complex, formation, volcanic rocks, basalts, siliceous rocks

CHEMISTRY FEATURES AND FORMATION IMPLEMENTS
OF THE PRE-CEMBRIAN PRYAZOVS'KIY OKTIABRS'KIY
INTRUSIVE COMPLEX (UKRAINIAN SHIELD)
A. Lysak¹, V. Pashchenko¹, B. Borodynja², O. Savina^1
1Ivan Franko National University of Lviv,
geological faculty, department of general and regional geology,
Hrushevskij Street, 4, 79005, Lviv, Ukraine
e-mail: zaggeol@franko.lviv.ua
²GP KP “Yuzhukrgeologiya”
Chernyshevskiy Street, 11, 49005, Dnepropetrovsk,
e-mail: boris21_63@mail.ru

The features of chemical of the October intrusive complex of Priazovye are considered, differences and similarities of features of chemical of his different phases are shown, drawn conclusion about belonging of him to the group of alkaligabroid formations.
Keywords: the Ukrainian shield, October complex, intrusive phases, chemical, formation.

SUTURE-STYLOLITE SEAMS IN THE UPPER CRETACEOUS
LIMESTONES FROM THE CRIMEA MOUNTAINS
AND THEIR ORIGIN
P. Bilonizhka¹, S. Kryzhevych^2
1Ivan Franko National University of Lviv,
geological faculty, department of mineralogy,
Hrushevskij Street, 4, 79005, Lviv, Ukraine,
e-mail: mineral@franko.lviv.ua
²Ivan Franko National University of Lviv,
geological faculty, department of historical geology and paleontology,
Hrushevskij Street, 4, 79005, Lviv, Ukraine,
e-mail: zaggeol@franko.lviv.ua

The main hypothesis of the suture-stylolite seams formation were reviewed. Suturestylolite seams in the Upper Cretaceous limestone from the right bank of the Bodrak River were described. Clay fraction from the limestones and clay film which covered stylolites were measured using x-ray diffraction. It was found that they have the same phase composition and mainly represented by montmorillonite. It is concluded that the suture-stylolite seams formed on the epigenesis stage as a result of penetration of atmospheric water in fractures which are common along the limestone layers, and their dissolution.
Key words: suture-stylolite seams, epigenesis, fractures, atmospheric water, limestone solution, Crimea Mountains.

ANALYSIS OF THE IMPACT OF L’VIV LANDFILL UPON
THE ENVIRONMENT
P. Voloshyn
Ivan Franko National Universityof Lviv,
geological faculty, department of ecological and engineering geology and hydrogeology,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
e-mail: petro.woloshyn@gmail.com

The results of investigations of soils, vegetation cover, surface and underground waters state within the landfill are presented. It is ascertained that surface and ground waters are most polluted environment components in the study area.
Key words: landfill, pollution, chemical and bacteriological composition, heavy metals, monitoring.

ACTIONS FOR THE GROUNDWATER PROTECTION AGAINST
DEPLETION AND POLLUTION
V. Kharkevich¹, S. Kryzhevych^2
1Ivan Franko National University of Lviv,
geological faculty, department of ecological and engineering geology and hydrogeology,
Hrushevskij Street, 4, 79005, Lviv, Ukraine,
e-mail: admingeo@franko.lviv.ua
²Ivan Franko National University of Lviv,
geological faculty, department of historical geology and paleontology,
Hrushevskij Street, 4, 79005, Lviv, Ukraine,
e-mail: zaggeol@franko.lviv.ua

In this article the measures for ground water protection against depletion and pollution are generalized. Preventive measuresagainst aquifer depletion are in fact so that during extraction of groundwater decline in the hole (in wells) were less acceptable. Actions of groundwater pollution are provided by strict implementation of laws, legal documents and sanitary protection of groundwater.
Key words: pollution, quality, water, law, requirements, water horizon.

THE PROBLEM OF LOCATING OF THE OIL-GAS LOWER
CRETACEOUS STRATA OF CRIMEA PLAINS REGION:
STRUCTURE-FACIAL AREAS, TYPES CUTS, INDICATIONS
AND CRITERIONS DISTINGUISHING
Ya. Tuzyak
Ivan Franko National University of Lviv,
geological faculty, department of historical geology and paleontology,
Hrushevskij Street, 4, 79005, Lviv, Ukraine,
e-mail: tuzyak@rambler.ru

The results of detail locating of the Lower Cretaceous strata of Crimea plains are given. Within the limits of structure-facial region and structure-facial subregion to complexes indications and criterions of structure-facial area are distinguishing. Types cuts and their concise character are given for each area.
Key words: structure-facial region, structure-facial subregion, structure-facial area, Crimea plain, Lower Cretaceous.

THE MATHEMATICS MODELLING IN SEISMOLOGY PROBLEMS
D. Malytskyi¹, V. Fourman^2
1Carpathians branch of Institute of geophysics the name S.I. Subbotin of NAS Ukraine,
Naukova Street, 3-a, Lvov, Ukraine,
е-mail: dmytro@cb-igph.lviv.ua
²Ivan Franko National University of Lviv,
geological faculty, department of physics of the Earth,
Hrushevskij Street, 4, 79005, Lviv, Ukraine,
e-mail: fourman@franko.lviv.ua

The solution of the direct problem for the displacement field on the free surface of layered isotropic medium using the matrix method is presented. The results of the direct problem are used to form the seismic moment tensor. The source time function of an earthquake is considered.
Key words: seismic field, seismic moment tensor, hearth of earthquake, isotropic environment.

COMBINATION OF THE KINEMATIC AND STRUCTURALPARAGENETIC
METHODS FOR STUDY THE EVOLUTION OF THE PALAEOSTRESS FIELDS OF ROCKS
IN THE UKRAINIAN CARPATHIANS
I. Bubniak¹, Yu. Vikhot^1,2, M. Nakapelukh^2
1Ivan Franko National University of Lviv,
geological faculty, department of physics of the Earth,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
e-mail: ibubniak@yahoo.com, yuvik@ukr.net
²Institute of Geophysics National Academy of science of Ukraine,
Palladin avenue, 32, 03680, Kyiv, Ukraine,
e-mail: nmsol@ukr.net

A detailed reconstruction the regional fields stress evolution of Skyba and Boryslav-Pokuttya nappes for prefolding, folding and postfolding stages of development of the Ukrainian Carpathians is presented. The chronological scale deformation modes with azimuths orientation of main axes palaeostress fields (σ1, σ2, σ3) during these stages were created using a complex application of structural-paragenetic and kinematic analyses. It has been proven that thrust shear stress was coeval with strike-slip that provided the rapid advancement of the thrust front. The influence of the Southern and Western Carpathians in the formation of Skyba nappe structure is shown in the creation of the stress fields with the axis of compression σ1 in the north-western direction.
Key words: the Ukrainian Carpathians, kinematic and structural-paragenetic methods, palaeostress field evolution, joint, slickenside, Skyba and Boryslav-Pokuttya nappes.

THERMOELECTRICE PROPERTIES OF CHALKOPYRITE
OF DEPOSITS OF YAREMCHANSKY HORIZONS
(SCUBOVA ZONE OF UKRAINIAN CARPATHIANS)
O. Kostyuk
Ivan Franko National University of Lviv,
geological faculty, department of petrography,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
e-mail: kostol@email.ua

Morphological properties of chalcopyrite from the rocks of Scubova zone of Ukrainian Carpathians were investigated. Thermoelectric properties and chemical composition of chalcopyrite were investigated too.
Key words: thermo-emf., сhalcopyrite, sulfides, siltstones.

FEATURES OF GEOLOGICAL STRUCTURE AND SOME
FORECASTING CRITERIA OF THE MANEVICHI AMBER
DISTRICT (VOLYN’)
S. Mamchur
Ivan Franko National University of Lviv,
geological faculty, department of general and regional geology,
Hrushevskij Street, 4, 79005, Lviv, Ukraine,
e-mail: zaggeol@franko.lviv.ua

Description of geological structure, lithologic composition and forecasting criteria of searches of amber deposits of Manevichi amber district are presented.
Key words: Manevichi amber district, amber, oligocen, intermontane assise, derivative parent deposits.

THE ROLE OF THE PRE-NEOGENE EROSION PROCESSES IN
FORMING FORMATION OF STRUCTURAL ELEMENTS OF OUTER
ZONE OF CARPATHIAN FOREDEEP
M. Andreychuk
Branch “Carpathian center” of DP of “Naukaneftegaz”
V. Velyky Street, 4, Lviv, Ukraine,
e-mail: viddil_ngg@i.ua

Briefly reviewed studies that were performed over the last decade by Ukrainian geologists. The role of the processes of denudation in the formation of the structural plan to the neohene External surface area of the Carpathian Foredeep Assumptions about the nature of erosion of Krukenytska. Influence of tectonic factors in generating the structural calculation to the neohene bed in the final stages of the Carpathian orogen.
Key words: sedimentation, paleogeomorphology, Neogene base, Krukenytska Depression, dislocation.

GEOECOLOGICAL CHARACTERISTIC UPLAND LAKES
IN THE AREA OF INFLUENCE PODOROZHNENSKE SULFUR CAREER
B. Kaminetska¹, A. Haydin², V. Dyakiv^1
1Ivan Franko National University of Lviv,
geological faculty, department of ecological and engineering geology
and hydrogeology,
Hrushevsky Street, 4, 79005, Lviv, Ukraine,
e-mail: dyakivw@yahoo.com
²Branch of the Ukrainian Academy of mining Sciences

For the first time on the basis of space photos analysis and during superficial testing the exact morphometrical and gidrochemical characteristics of mountainous lakes of the 1st dump Podorojniansky sulphuric quarry were established. The main factors of explored reservoirs and their modern geoecological state are the only mechanism of piling accepted for a period of extractive work at the dump № 1, filtering qualities and phytophilous of dump breeds, processes of drain self-organization, exogenous geological processes (slumps, doslocations, landslide). Linear and sloping erosion activization might result in degradation of reservoirs what can include water column catchment, edge destruction and surface flow power increase, mechanical suffosion with strengthening of filtration and underground zones of relief power increase of.
Key words: sulphuric quarry, dump, mountainous lakes, Google Earth photos, morphometrical and gidrochemical characteristics, geoecological state.

THE 300TH ANNIVERSARY OF THE BIRTH OF MIKHAIL VASILYEVICH LOMONOSOV
O. Matkovskyi, P. Bilonizhka

Y.Z. KRUPSKIY (TO 70 YEARS FROM BIRTH)
R. Leshuh, B. Polyniak, P. Chepil’

DANYLO MYKHAYLOVYCH DRYGANT: 50 YEARS OF CREATIVE WORK
AND DISCOVERIES (TO SEVENTIETH ANNIVERSARY)
S. Bakayeva

HENNADIJ OLEKSANDROVYCH LUN’OV
(OF BLESSED MEMORY OF THE TEACHER AND COMRADE)
M. Pavlun’, Yu. Lyakhov, O. Shvayevs’kij, A. Sivoronov, O. Hayovs’kyj, S. Tsikhon’,
H. Yacenko

RESULTS OF THE THIRD INTERNATIONAL GEOLOGICAL STUDENT CONFERENCE
I. Bubniak, Tsikhon’, O. Pavluk, S. Kril

IV INTERNATIONAL CONFERENCE “GEOLOGICAL FIELD PRACTICE
IN THE SYSTEM OF HIGHER EDUCATION”
P. Bilonizka, L. Generalova

SECOND INTERNATIONAL CONFERENCE “GEOPHYSICAL STUDIES AND
MODELING OF PHYSICAL FIELDS OF EARTH”
Yu. Datsyuk

MEETINGS WITH ALUMNI IN 1972
V. Pashchenko

MEETING AFTER THIRTY YEARS
P. Bilonizka

RUSSIAN-UKRAINIAN DICTIONARY of GEOLOGICAL TERMINOLOGY
R. Vovchenko

SOLEMN ACADEMY DEVOTED TO MEMORY OF PROMINENT SCIENTIST-GEOLOGIST GEOLOGISTS DMITRY REZVOY
A. Sivoronov, L. Generalova

NATIONAL CONFERENCE “COMPLEX STRATIGRAPHIC METHOD IN
TRACING MINERALS IN UKRAINE PHANEROZOIC SEDIMENTARY COVER”
A. Danyliv

STUDENTS THAT WERE GRADUATED FROM GEOLOGY DEPARTMENT
IVAN FRANKO NATIONAL UNIVERSITY OF L’VIV AT 2012 YEAR
P. Bilonizhka, O. Polubichko