IRON-ORE FORMATIONS OF THE GREENSTONE COMPLEXES OF THE
EAST–EUROPEAN PLATFORM (SYSTEMATIZATION AND GENESIS)
A. Sivoronov
Ivan Franko National University of Lviv
Hrushevskij Str. 4, Lviv, 79005, e-mail: zaggeol@franko.lviv.ua

Analysis of distribution of iron-ore formations in the formation sets of the greenstone belts is conducted and determined, that these formations in structures with the monocyclic formation sets of the type of “M” (lower ultramafic–mafic formations) with contrasting and by successive combination of formations are prevailed. Iron-ore formations of the type of Kryvyi Rih are appeared in volcanic part of the section of jaspilite-tholeiit type of formation. Formations which include ferruginous quartzites with acid effusive rocks are corresponded exceptionally to the formation sets of the type of “M” and, they are or itself contrasting (jaspilite-rhyolite-dacite formation), or are in contrasting combination with komatiite or komatiitetholeiite formations. It is indicated that iron accumulation in sedimentary parts of the section is related to the certain types of volcanic formation sets and thus with the general process of evolution of magmatism of the greenstone belts.
Key words: greenstone belts, formation sets, iron-ore formations, volcanic formations, sedimentary formations, formation types, formations of the type of Kryvyi Rih.

PLACE OF KRYVYI RIH AND BILOZERKA IRON-CONTAINING SECTIONS IN
THE STRUCTURAL-FORMATION COMPLEXES
OF THE UKRAINIAN SHIELD
I. Paran'ko
Kryvyi Rih State Pedagogical University
Gagarin Av. 54, Kryvyi Rih, 50086, е-mail: paranko@mail.ru

Iron-containing section of Kryvyi Rih structure is represented by the rocks of meta¬psephite-psammite-pellite, metakomatiite and ferrous-siliceous-schist formational types. The necessity of distinguishing of this section from the granitoid-metasedimentary typical
structural-formational complex is grounded. It is suggested to attribute him (together with the section of Bilozirka structure, which is similar on formational structure) to the tonalitegreenstone structural-formational complex.
Key words: structural-formational complex, rock complex, concrete formation, formational type, iron-containing sections, Kryvyi Rih structure, Bilozerka structure, Ukrainian Shield.

PECULIARITIES OF LITHOSPHERE DEPTH STRUCTURE PART OF MANTLE
OF OLD SHIELDS AND PLATFORMS FROM POINT OF POTENTIAL DIAMONDIFEROUSNESS
Yu. Fedoryshyn, M. Yakovenko, Yu. Myschyshyn, N. Triska
Ukrainian State Geological Research Institute (UkrSGRI) Lviv Branch
Pasichna Str. 38а, Lviv, 79038, e-mail: lv_ukrdgri@polynet.lviv.ua
myroslavakoshil@ukr.net
geologist@bigmir.net

The method of discriminate between lithosphere segments (megablocks, blocks) within Precambrian shields and platforms after the completeness of evolution, which is the function of intensity and duration of process of the fluid mantle degassing, a depletion of lithospheric mantle and expressed by thickness of lithosphere and composition of the Earth's crust is considered. The analysis of mantle part of lithosphere and asthenosphere, which is based on modern achievements of petrology and experimental mineralogy in the form of wide spectrum of petrological-geochemical data, is consolidated to whole in a number of logicale and enough substantiated positions. In an aggregate with deep geophysical researches these information can be successfully used for prognostication of diamondiferousness of old shields (platforms), reveal potentially of diamondiferous areas (natural boundaries of the kimberlite fields) and areas of localization of groups of solids (separate solids) depending on the scale of researches and detailed of used materials.
Key words: old shields, megablocks, blocks, lithosphere, Earth’s crust, upper mantle, asthenosphere, depth structure of lithosphere, diamondiferousness, diamondiferous kimberlite melt.

HEAT TRANSFERING AND HEAT FLOW DIFFUSION
IN THE EARTH’S MANTLE CONVECTION PLUMES
V. Fourman
Ivan Franko National University of Lviv
Hrushevskij Str. 4, Lviv, 79005, е-mail: fourman@franko.lviv.ua

A model of thermal diffusion of mantle plumes, indicating that stem plumes are destroyed faster than their caps as a result of thermal diffusion. This may explain the recent results seysmotomographic studies of mantle plumes that are not show the exponent-governmental legs mantle plumes at the mid depths. The shift and distortion of a mantles plume resulting convection currents did not change significantly the features of the thermal evolution of mantle plumes.
Key words: mantle convection, evolution, plume, diffusion

Is ANTHROPOGENIC GEOLOGY ALTERNATIVE TO QUATERNARY GEOLOGY
OR IS IT A NEW SCIENTIFIC TREND?
I. Paran’ko¹, Ye. Slyvko², M. Pavlun’², A. Sivoronov^2
1Kryvyi Rih State Pedagogical University
Gagarin Av. 54, Kryvyi Rih, 5008, e-mail: paranko@mail.ru
²Ivan Franko National University of Lviv
Hrushevskij Str. 4, Lviv, 79005, e-mail: zaggeol@franko.lviv.ua

Difference between Anthropogenic Geology and traditional Quaternary Geology has been ground in the article. Anthropogenic Geology is the new scientific trend, the purpose of which is the comprehensive study of properties, structure, conformities to the law of development of the natural-anthropogenic (natural-technogenic) geological systems, while quaternary geology studies the natural geological systems, formed during the Quaternary period of the Earth’s development. One of the tasks of Anthropogenic Geology is the development of geologicaleconomic conformities to the law of the world raw materials sources forming and ground of financial viability and efficiency of the mineral resources use.
Keywords: Anthropogenic Geology, Quaternary Geology, natural system, natural-technogenic system, technogenesis.

EARTHLOGY AS NEW SCIENTIFIC DIRECTION IN GEOECOLOGY
G. Rud’ko
Geological Survey of Ukraine
State Committee of Ukraine for Mineral Reserves
Kutuzova Ave, 18/7, of. 816, Kyiv, 01133, e-mail: scmr@dkz.gov.ua

The fundamental problems concerning the modern state of Earth as a planet that experiences the period of environmental crisis are elaborated. Researches about the evaluation of natural-resource potential and scopes of its using by humanity are conducted. The strategic aspects of influencing of global rise of the temperature were analyzed. Technological principles of the management of СО2 content in the atmosphere of Earth are shown. The scenarios of development of Earth are presented in the technogenic trajectory of humanity evolution.
Key words: biosphere, environmental crisis, technogenesis , natural-resource potential, global rise of the temperature.

GEOLOGICAL STRUCTURE AND MODERN GEOECOLOGICAL STATE OF
THE SOLOTVYNO SALT DEPOSIT (TRANSCARPHATIAN)
V. Dyakiv, P. Bilonizhka
Ivan Franko National University of Lviv
Hrushevskij Str. 4, Lviv, 79005, e-mail: dyakivw@yahoo.com

Geological structure, mineralogical and lithological composition, modern geoecological state, hydrogeological and mine-geological condition of the Solotvyno salt deposit (Transcarpathians) is presented. Activation factors of geodynamic processes by forming of salt-diapir structure and displays of the salt karst in the process of exploration of deposit are considered. Mastering of deposit resources in the future is possible by three methods: by the gasket of a new mine, building of quarry and salt-brine mining method. Conditions and errors, are definite which it is necessary to take into account in future by planning and building of new mines within the limits of the Solotvyno deposit or similar geological structures of the Carpathians region.
Keywords: The Solotvyno salt deposit, geoecological state, mine-geological and hydrogeological terms, mineral composition, salt karst.

ECONOMIC ACTIVITY AND GEOECOLOGY OF THE BLACK SEA
V. Gevork’ian
Institute of Geological Sciences of the National Academy of Sciences of Ukraine
O. Gonchar Str., 55-B, Kyiv, e-mail: info@igs-nas.org.ua

The problems of the environmental protection of the Azov-Black Sea Basin related to the exploitation of the mineral resources of the sea bottom are considered in the paper. The top importance in the assessment of environmental situation in a marine aquatory belongs to the geological substratum as an accumulator of all pollutants from the atmosphere, water layers, river system, ships, oil platforms as well as from the natural geological phenomena. Some conceptual positions of geoecological control are justified and the certain hierarchy of the investigations is supposed that is based over the landscape geoecological mapping. It is shown that many problems of geoecology both in the methods and so in the receiving of the reliable information, distribution of practical recommendations and forecast estimations can be solved only through using of manned underwater vehicles. The results of the technical state inspection of the deep water canalization systems at the Crimean-Caucasus coast and main pipelines in the northwestern part of the Black Sea are given. It is determined that the natural territorial complexes of the sea bottom are the most important targets for the ecological examination. The integration of the methods solving regional and local problems is able to give the most essential results for the creation of the efficient environmental control and protection system.
Key words: abyssal fluids, bottom deposits, substratum, dumping.

THERMOPHYSICAL CHARACHTERISTIC OF GRANITOIDS OF THE VOLYN'
REGION AS CRITERION OF ESTIMATION OF THEIR FITNESS FOR
BURIAL PLACE OF RADIO-ACTIVE WASTES
L. Kuziv, M. Tolstoj
Institute of geological sciences of the National academy of sciences of Ukraine
Gonchar Str., 55б, Kyiv, e-mail: Liliana_k@ukr.net

The summarized data of the thermal conductivity coefficient dependences of the mineral composition, structure, texture and other granitoids properties of the Volyn region are presented. The changing of the thermal conductivity, thermal diffusivity and specific heat coefficients under the influence of the high pressure and temperature, that is very actual for the geological system of the waste disposal and others dangerous substances are analyzed here.
Key words: system of burial place, radio-active wastes, coefficient of heat conductivity, petrotypes, granitoids, convection, permeability.

STRUCTURAL FEATURES OF THE ORIVSKA AND SKOLIVSKA THUST
SHEETS OF THE SKYBOVA STRUCTURAL-FACIES ZONE IN MIDDLE PART
OF THE BASIN PRUT RIVER
(THE UKRAINIAN CARPATHIANS)
L. Generalova
Ivan Franko National University of Lviv
Hrushevskij Str. 4, Lviv, 79005, e-mail: zaggeol@franko.lviv.ua

Joint paragenesis are described and types of folds higher orders of the Striyska suite of the Orivska and Scolivska thust sheets of the Scybova nappe of the Ukrainian Carpathians in middle part of the basin Prut river are charactarized in details.
Key words: Scybova structural-facies zone, Orivska thust sheet, Scolivska thust sheet, joints, folds, scale, structural paragenesis.

SOME ASPECTS OF GEOLOGICAL CONSTRUCTION AND MINERAL COMPOSITION
OF FLISH FORMATION IN R. BODRAK TERRITORY (CRIMEA)
P. Bilonizhka, L. Generalova, O. Shvaevskiy
Ivan Franko National University of Lviv
Hrushevskij Str. 4, Lviv, 79005, e-mail: mineral@franko.lviv.ua

The problem of geological structure, mineral composition, paleogeographical condition of sedimentation and post sedimentation changes in Crimea flysch formation have been considered. Complicated geological structure of flysch and fossilized fauna rareness are the main causes of absence its generally accepted stratigraphical scheme. Phase composition of clay minerals from argillites, clays and other rocks of Dzhydairska, Menderska and Verhnjotavrijska sequences on r. Bodrak basin was studied by X-ray analysis. Clay minerals are presented by dioctahedral hydromica, Fe- and Md-Fe chloriteses with admixture of mixed-layer clay minerals phases hydromica – smectite, hydromica – chlorite and kaolinite. The thin layers of betonite clays were discovered at verhnjotavrijska sequences. There were composed mainly of smectite and dickite and nacrite. The betonite clays were formed due to volcanic ashes decomposition, and dickite and nacrite were formed from lowtemperature hydrothermal solutions. The considerable changing in clay minerals composition were determined in rock of Menderska sequences clays near magmatic body and faults.
Key words: flysch, rock, clay mineral, genesis, generating conditions, Crimea.

SPACE CHANGEABILITY OF THE DECREPTOMETRIC PARAMETERS OF
QUARTZ FROM SAULIAK GOLD DEPOSIT (RAKHIV ORE AREA, TRANSCARPATHIAN REGION)
А. Horodechnyy, T. Oliynyk, I. Popivniak, S. Tsikhon’, V. Marusiak
Ivan Franko National University of Lviv
Hrushevskij Str. 4, Lviv, 79005, e-mail: mineral@franko.lviv.ua

On the basis of creation and detailed analysis of lineal decreptometric models space changeability of some decreptometric parameters of Quartz from Sauliak gold deposit was investigated. Different values of these parameters in ore body and in barren rocks were determined. We suppose that ore process and tectonic movement in ore zone ware synchronized in time.
Key words: Quartz, decreptometric analysis, ore body, modeling, gold deposit, Sauliak.

SOME ELECTRICAL PECULIARITIES OF ARSENOPIRITE AS TYPOMORPHIC
CRITERION OF SEARCH AND AN ASTIMATION OF GOLD MINERALIZATION
IN FOLDED CARBON-BEARING WEAKLY METAMORPHIZED
SEDIMENTARY ROCKS
(NAGOL'NIY MOUNTAIN-RIDGE, DONBAS)
O. Lytvynovych, V. Ekhivanov, Yu. Pakhnyuschyi, V. Stepanov, O. Tsaban,
O. Shvaevskyi, O. Savina
Ivan Franko National University of Lviv
Hrushevskij Str. 4, Lviv, 79005, е-mail: geomin@geof.franko.lviv.ua

Based on a morphogenetic and electrical features of arsenopyrite, it has been concluded that within the Bobrykiv ore field the express mapping of the potentially ore-bearing zones can be carried out by only certain mineralogical-physical parameters of arsenopyrite.
Key words: arsenopyrite, morphogenetic type, thermoelectrical force, coefficient of thermoelectrical force, auriferousity.

ROLE OF MINERALOGICAL RESEARCHES IN STUDY OF
GEOLOGICAL STRUCTURE OF COUNTRY BETWEEN OF BODRAK
AND KACHA (CRIMEA)
P. Bilonizhka
Ivan Franko National University of Lviv
Hrushevskij Str. 4, Lviv, 79005, e-mail: mineral@franko.lviv.ua

The results of long-term mineralogical researches of the stratified silicates are generalized in the deposits of siltages of country between of Bodrak and Kacha. In flyshe of Tauric series the thin are exposed prosloy bentonyts clays, vein of yarosite, dikkit, nakrite and their phase composition is studied. After information of research of clay minerals in the nyzhnemelovykh deposits, stratygrafycheskoe position of mangushskoy of retinue is specified. The origin of styazhenyy flints and stylolytovykh stitches is explored at verkhneturonskykh limestones. As a result of study of the clay minerals abstracted from marls and limestones of overhead chalk and paleogene, it is set that they montmoryllonytom is represented mainly with the admixture of gydroslyudy, khloryta, sometimes tseolytov klynoptylolytgeylandytovoy groups. It is found out that accumulations of glaukonyta, and placed and fosforyta on the uneven, washed out surfaces of marls of senomanskogo, maastrykhtskogo, tanetskogo and limestones of turonskogo and Danish tiers, related to the displays of submarine vulkanyzma. The conducted mineralogical researches allowed more in detail to experience history of geological development of district.
Keywords: siltages, stratified silicates, mangushskaya svyta, stalolytovye stitches, styazhenyya flints, display of vulkanyzma, history of geological development, Crimea.

PROBLEMS OF PRACTICE USING OF THE ABIOGENIC THEORY
OF HYDROCARBONS GENESIS
V. Guliy, G. Lepigov
Ukrainian State Geological Prospecting Institute
Avtozavodska Str., 78, Kyiv, 04114, е-mail: vgul@ukr.net

Initial points of the system of knowledge on abiogenic genesis of hydrocarbons and its reflection on possibilities of solving practical problems of safety coal mining and creation of scientific basement for hydrocarbons exploring are given in this article. Evidences on natural methane flows of deep origin, which can initiate big scale blasts, as well as possibilities of using of geochemical and isotopic marks for ” young gas” to select promising parts during hydrocarbons exploring, are shown here.
Key words: abiogenic genesis of hydrocarbons, young gas, isotops, coal deposit, oil and gas fields.

PALYNOLOGICAL MATERIALS FROM DEPOSITS MESOZOIC STRATIGRAPHY
OF THE RIVER VALLEY OF THE ZOLOTA LYPA (PODILLYA)
O. Shevchuk
Institute of Geological Science of the NASU
O. Gonchar Str., 55 b, Kyiv, 01054

The results of detailed palynological studies of Jurassic sediments (Bajocian, Tithonian) and Cretaceous (Cenomanian, Turonian) sections near Zavadivka and Korzhova villages in Zolota Lypa river valley, which is located within the Volyno-Podillya plate. The four sporepollen complex and four complex dinocysts: Bajocian, Tithonian, Cenomanian, Turonian are described. Based on the palynological data for the first time is proven the position of the border between Jurassic and Paleozoic (Devonian)and between Cretaceous and Jurassic in the studied succession.
Key words: spores, pollen, dinocysts, Jurassic and Cretaceous sediments, biostratigraphia, Podillya.

FORMATION CONDITIONS OF THE n8 COAL BED OF THE MINE № 1 NOVOVOLYNSKA
OF THE LVIV-VOLYN BASIN BASED
ON PALYNOLOGICAL DATA
A. Ivanina, E. Gonyk
Ivan Franko National University of Lviv
Hrushevskij Str. 4, Lviv, 79005, e-mail: ant_iv@mail.ru

Investigations of dispersed organic matter of coal bed n8 of the Lviv-Volyn basin by means of palynoorictocenosis is conducted for the first time. Systematic composition of spores and pollen is studied and different types of palynoorictocenosis are determined. Based on these data there is reconstructed the paleo-vegetation and it is distinguished the forming phases of coal peat bog of coal bed.
Key words: palynoorictocenosis, dispersed organic matter, spores and pollen, coal bed n8, mine N 1 Novovolynska, lycosporic, densosporic and intermediate phases.

GENETIC TYPES OF COALBED SPLITTINGS IN THE LVIV-VOLYN
COAL BASIN
M. Matrofailo
Institute of Geology and Geochemistry of Combustible Minerals
of National Academy of Sciences of Ukraine
Naukova Str. 3a, Lviv, 79060, e-mail: igggk@mail.lviv.ua

On the basis of morphostructural analysis and conducted paleoreconstruction of the primary thickness of the coal seams and coal-free deposits substituting them along the strike in the zone of splittings, and taking into account the coefficients of rock consolidation, it was possible to determine tectonic and atectonic types of splittings. A morphostructural analysis of the coal fields of the basin has allowed us to reveal that local splittings of tectonic nature are prevailing, and their formation was caused by consedimentational differentiated tectonic movements of the basement promoting subsidence and uplifting of some sites of the territory of coal formation. In shape and origin, bifurcation of coalbeds is prevailing in the coal-bearing formation of the basin and is characterized, as a rule, by dividing of a solid bed into two units. Cades of complicated bifurcation when the bed is splitted into three or more coal units are in limited quantities. Data expounded in the paper are of great significance for determination of special features of the structure, formation conditions and comparative analysis of coal-bearing formations of the Lviv-Volyn Basin and other typical coal basins and for the development of the methods of morphological analysis of coal deposits.
Key words: morphology, tectonic, atectonic and Z-like splittings, bifurcation, contraction coefficient, morphostructural analysis, paleoreconstruction.

ROLE OF FLINTS IN THE KNOWLEDGE OF GEOLOGY AND ARCHAEOLOGY
OF EAST-EUROPEAN PLATFORM SOUTH-WESTERN PART
G. Yatsenko¹, V. Yatsenko^2
1Ivan Franko National University of Lviv
Hrushevskij Str. 4, Lviv, 79005, e-mail: Yatsenko1941@list.ru
²Institute of Environmental Geochemistry of NASU
Acad. Palladin Av. 34a, Kyiv, 03142

The studied flints on territorial, age, colour and luminescent peculiarities are subdivided into genetic groups. Their connections with certain geological and ore formations are shown. It is found out that flints for obtain of goods had been worked up not only by one method “stone on a stone”, both more difficult methods and other hard materials (possibly, diamond) had been applied.
Key words: flint, technology of working up, Mesolithic, Neolithic stage, East-European Platform, archaeology.

MINERALOGICAL PROPERTIES OF FLINT RAW MATERIAL
FOR PALEOLITHIC TOOLS IN PODILLJA REGION
V. Fourman
Ivan Franko National University of Lviv
Hrushevskij Str. 4, Lviv, 79005, е-mail: fourman@franko.lviv.ua

A review of the properties of flints materials for Paleolithic tools near Dnister and on the Podillja region. It is noted that the knowledge of the properties stone for tools paleolithic, acquaintance with the diversity of its properties and parameters were the basis of the primary mineralogy of representations since the choice of raw materials in the Paleolithiccal time was of decisive importance in the close dependence of raw materials and types of manufactured of his tools. Activity of recycling raw stone represents one of the most important channels of intensive learning about the world, the accumulation of positive knowledge and the future establishment of the primary scientific ideas about the structure of matter.
Key words: stone tools, flint, flint raw materials, pebbles.

THE GEOLOGICAL PAST OF UNIQUE ARCHEOLOGICAL MONUMENT
OF UKRAINE “KAMJANA MOGYLA”
V. Manyuk
Dnipropetrovsk Oles Gonchar National University
K. Marx Str. 36, Dnipropetrovsk, 49066, e-mail: manuk-geo@mail.ru

During realization of auditing inspection of geological monuments of a nature in the Zaporozhye area in number of objects of a geological heritage the hill from глыб quartz sandstones "Kamjana Mogyla " with world famous rock paintings and figures (petrogliyphs) is included. The problem of genesis of a unique monument of a nature and archeology (as sandstone’s block, and hill) is considered.
Key words: Geological monument, petrogliph, geological heritage, sandstone, Kamjana Mogyla, palaeolith, genesis.

THE PARADIGM CHANGE IN THE GEOLOGY OF XXCENTURY:
RETROSPECTION AND PERSPECTION(LULLABY FOR MOWGLI)
I. Popadyuk
SPK-Geoservice Ltd
Kharkivskie shosse 144-V, Kyiv, 02091, e-mail: popadyuk123@yandex.ru

The paradigm change in the modern geology was triggered with plate tectonic concept in 70-th of the last century. Retrospective analysis reveals that paradigm shift has occurred when a “new” concept interpreting a new body of data acquired beyond the scope of the “old” concept has incorporated the data massif from the “old” concept domain overprinting it at “new” concept pattern.
Key words: Geology, Philosophy, concept, paradigm

International scientific conference
“GEOPHYSICAL STUDIES AND MODELING OF PHYSICAL FIELDS OF EARTH”
Yu. Datsyuk
Ivan Franko Lviv National University
Hrushevskij Str., 4, Lviv, 79005, e-mail: yudat@ukr.net

LIST OF STUDENTS THAT WERE GRADUATED FROM
IVAN FRANKO NATIONAL UNIVERSITY OF L’VIV
AT 2010 YEAR