̲ÍÅÐÀËÎò×ÍÈÉ ÇÁ²ÐÍÈÊ 2002 ð. ¹ 52, âèï. 1
Ñ. 4–11
The past, contemporary
and the future of the academician Yevhen Lazarenko Mineralogical museum of
the Lviv National University (regarding the 150th anniversary of its foundation)
O. Matkovs’kyi, L.
Volkova
E-mail: geomin@geof.franko.lviv.ua
The activity of the
academician Yevhen Lazarenko Mineralogical museum of the Ivan Franko National
University of Lviv during 150 year of its official existence has been analysed.
The role of different persons in museum development as well as museum’s tasks
for future has been noted.
Key words: mineralogical museum, Yevhen
Lazarenko, collections, museum structure, stationary and thematic expositional
fond.
Ñ. 12–14
Museum business and the problem of mineral variety in Ukraine
V. Pavlyshyn
E-mail: pavlyshin@mail.univ.kiev.ua
The attention
is concentrated on a qualitatively low level of development of Ukrainian
mineralogical museums, which in Europe and in the world are poorly known, are
poorly active in exhibition and scientific activity, especially abroad, are not
able (or do not want) to earn money. The attention also on development
extremely urgent for Ukraine of a mineral variety problem is inverted, as per
past years due to its ignoring Ukraine very much has suffered.
Key words: museums, museum business, mineralogical museums
of Ukraine, mineral variety, program of development and preservation of a
mineral variety.
Ñ. 15–18
To 195th anniversary of Mineralogical museum of V.N. Karazin
National University of Kharkiv
P. Zaryts’kyi
The article deals with the history
of the foundation and development of one of the oldest and largest mineralogy
museums of Ukrainian universities. The history of the museum started in 1807,
when it was founded, and going on now, when it has become the mineralogy sector
of the Kharkiv National University Museum of Nature.
Key words: mineralogy,
mineralogical study, mineralogical muzeum, exhibit, collection, meteorites,
synthetic minerals.
Ñ. 19–23
History, modern condition and perspectives of development
of National Mining University Mineralogical-Geological museum
V. Boyko
National Mining
University, Karl Marx Av., 19. UA – 49027 Dnipropetrovs’k, Ukraine
E-mail: BaranovP@nmuu.dp.ua
The article deals
with the history of foundation, further development and modern condition of
geological-mineralogical museum in National Mining University.
Key words: geological-mineralogical
museum, minerals, rocks, gemmology, gemstones, Dnipropetrovs’k.
Ñ. 24–28
Mineralogical museum of Odesa University, its
significance in preparation of specialists-geologists
V. Usenko, O.
Chepizhko, V. Kadurin, S. Kadurin
I.I. Mechnikov
National University of Odesa, Dvoryans’ka St., 2. UA – 65100 Odesa, Ukraine
Å-mail: chepodes@ukr.net; kadurin@paco.net
Mineralogical museums are the major objects of
information storage and knowledge ordering. They carry out the basic functions
– educational and scientific. Odessa National University mineralogical museum
was formed as educating-scientific structure of geological branch of the
University. The modern expositions of the museum are submitted by the following
sections: regular educational collections of minerals and rocks; regional
collections of minerals and rocks of CIS and Ukraine; unique scientific
collection of iron-manganese concretions and rocks from the bottom of the Indian
and Pacific oceans; minerals collection of Odessa underground cavities;
collections of minerals from human organism, artificial minerals, and also
assembly of gems, ancient books and devices. The special place is occupied by
the collection of meteorites.
Key words: mineralogical
museum, minerals, rocks, gemstones, Odesa.
Ñ. 29–35
Unique
collection of the Museum of precious and decorative stones – national property
of the Ukrainian people
I. Vasylyshyn, V. Lyzun
Museum of
Precious and Decorative Stones, Marx St., 58. UA – 12100 Volodars’k-Volyns’kyi,
Ukraine
The mineralogical collection, on the basis of which the
Museum of precious and decorative stones has been created, is mainly samples of
rocks and minerals from chamber pegmatites of the Volynsk morion deposit. This
is unique in Ukraine the chamber pegmatites
deposit on which the unique crystals of quartz, topaz and beryl are extracted.
Key words: Volynsk deposit, museum, mineralogical
collection, chamber pegmatites, topaz, beryl, morion.
Ñ. 36–45
CRIMEA
NATURE MINERALOGICAL MEMORIALS
Î. Tyshchenko
Crimean Branch of
UkrSGRI, Kirov Av., 47/2. UA – 95017 Simferopol’, Ukraine
Short
geological and mineralogical descriptions of some Crimean geologic objects,
which apply for a role of nature mineralogical memorials, are given.
Key words: mineralogical nature memorials, Ayudag,
Bakla, Karadag, Kerch iron-ore basin, Pershotravnevyi
quarry, acid lake.
Ñ. 46–47
MINERALOGICAL MUSEUM OF THE ST.-PETERSBURG STATE UNIVERSITY TO-DAY AND
IN FUTURE
G. Anastasenko, O. Golyns’ka
Mineralogical Museum of the St.-Petersburg State University,
Universytets’ka Embankment, 7/9. RU – 199034
St.-Petersburg, Russian Federation
E-mail: mm2002@AA5709.spb.edu
Some problems
of the preservation, systematisation, using and popularisation of the
St.-Petersburg State University mineralogical Museum collections has been
studied.
Key words: mineral, museum exposition,
collection systematisation.
Ñ. 48–50
significance of mineralogical museum
in preparation of the experts-ecologists
A. Piznyur, P. Nikolenko
E-mail: ecogeo@franko.lviv.ua
The study of
rocks composition is importance assignment of ecology because of highly active
processes of minerals chemical destruction in the crusts of weathering, the
migration of chemical elements form the halo of pollution. Therefore all the
stages of study of ecology carry out on basis of mineralogical museum.
Key words: ecology,
migration, crust of weathering, technogenic load.
Ñ. 51–54
O. Shchyrytsya1,
L.
Shchyrytsya2
The various aspects of bowel public protection in
Ukraine are considered. Main among them are: preservation of bowel with their
riches and environmental sites of the Earth’s crust in a primary kind;
protection and rational use of bowel with a variety of minerals during
production of mineral raw material and in the cases which have been not
connected to production process; protection of environment nature on mineral
deposits and decision of difficult tasks connected to the most vital ecological
problems.
Key words: public protection of bowel, nature protection
sciences, mineral raw material, Ukraine.
Ñ. 55–60
PECULIARITIES OF NATIVE COPPER OF UKRAINE
V. Kvasnytsya1, I. Kvasnytsya2
1Institute
of Geochemistry, Mineralogy and Ore Formation of NASU, Palladin Av., 34. UA-03680 Kyiv, Ukraine
E-mail: vmkvas@i.com.ua
2Taras Shevchenko National
University of Kyiv,
Vasyl’kivs’ka St., 90. UA-01022
Kyiv, Ukraine
Morphology, chemical composition and
mineral associations of native copper from the main ore regions of Ukraine
are analysed.
Ñ. 61–67
G. Kul’chyts’ka, V. Mel’nykov
Institute of
Geochemistry, Mineralogy and Ore Formation of NASU, Palladin Av., 34. UA –
03680 Kyiv, Ukraine
E-mail: annk@viptelecom.net
Fluorite types that differ by inclusions of mineral-forming environment
– from salt and silica melts to water solutions – are defined in syenites of
the Azov stock, where zircon-rare-earth deposit of the same name is located. Variety
of fluorite types is explained by the influence of the layering in silica-salt
melt and melt-brine.
Key words: fluorite, inclusion of melt, melt-brine,
liquation, layering.
Ñ. 68–73
THERMOBAROGEOCHEMICAL GROUNDS OF THE UKRAINE GOLD-BEARING
ENDOGENOUS DEPOSITS ORE-FORMATIONAL BELONGING: THEORETICAL AND METHODOLOGICAL
ASPECTS
Yu. Lyakhov, M. Pavlun
Ivan Franko National University of Lviv, Hrushevskogo St.
4, UA – 79005 Lviv, Ukraine
Some questions in the new
field of the ore-formational analysis – thermobarogeochemical modeling,
diagnosis and forecasting of the gold-bearing formations are considered.
Key words: formation,
thermobarogeochemical modeling, gold, fluid inclusions.
Ñ. 74–82
Gold from the sedimentary
complexes of the Ukrainian Carpathians
M. Koval’chuk
The morphological
characteristic of gold from heteroaged sedimentary complexes of the Ukrainian
Carpathians is presented. Chronous, spaces and lithofacial distribution of gold
in sedimentary complexes and the peculiarities of its morphology, inner
structure, granulometry and chemical composition are connected. On the base of
gold study the morphological classification is presented.
Key words: gold, morphology, granulometry,
chemical composition, morphological classification, sedimentary complexes,
Ukrainian Carpathians.
Ñ. 83–88
MORPHOLOGY AND GRANULOMETRY AS THE MAIN TYPOMORPHIC FEATURES
OF DIAMONDS
O. Palkina
Crimean Branch of UkrSGRI, Kirov Av., 47/2, UA – 95017
Simferopol, Ukraine
E-mail: imr@utel.net.ua
The
analysis of typomorphic features of diamonds sets incorporated to genetic, territorial or age attributes, enables to find
out a high degree of information of such typomorphic features as crystal
habitus and its granulometric distribution, and testifies to their close
connection.
Key
words: diamond, morphology, typomorphism, kimberlite,
metamorphic rocks, placers, Ukraine.
Ñ. 89–98
Peculiarities
of serpentinization and carbonatization of Pryazovian kimberlites
Yu. Fedoryshyn, S. Bekesha, S.
Biruk
Research Centre of the Ukrainian Ministry of Education and Science, Stepana Bandery St. 12, UA – 79013
Lviv, Ukraine
On an example of the kimberlitic pipes Yuzhna and
Novolaspins’ka three stages of serpentinization of the kimberlites from
Pryazovian region have been characterised. The change of this process with
depth has been traced. Peculiarities of carbonatization of Pryazovian
kimberlitic rocks are given.
Key words: kimberlitic pipe, serpentinization,
carbonatization, lizardite, serpophite, calcite, microelements.
Ñ. 99–104
Ì. Zintchouk1, D. Kotel’nikov1, A. Gorshkov2, A. Rotman1, M. Zintchouk1,
Yu. Stegnyts’kyi1, N. Solodkova3
1Yakutian Geological Enterprise of Exploration, Research &
Development (YaGEER&D) CNIGRI “ALROSA” Co. Ltd. Chernyshevsky Sh. 7. RU –
678170, Mirny, Saha, Russian Federation
E-mail: adm.cnigri@alrosa-mir.ru; yanigp@mail.ru
2Institute of Geology of Ore Deposits,
Petrography, Mineralogy and Geochemistry, Staromonetny
Per. 35. RU – 109017, Moscow,
Russian Federation
3Geology Department of Moscow State
University, Vorobyovy Hills. RU – 119992, Moscow,
Russian Federation
Arising on olivine serpentine is one of the earliest
minerals in the process of hypergene-metasomatic transformation of kimberlites.
With lowering of thermobarometric parameters and change of hydrogeochemical conditions
towards the increase of minerogenesis system Eh, serpentine successively
transforms into saponite. Regulated mixed-layered formation of
lizardite-saponite type arises as metastable phase, therewith, in interlayers
of autolith kimberlite breccia, characterised by hampered water exchange with
host rocks.
Key words: kimberlite, autolith kimberlite breccia, minerogenesis,
layer minerals, mixed-layered formation.
Ñ. 105–106
REE IN AMPHIBOLES:
GENERAL DISTRIBUTION REGULARITIES
F. Lesnov
Institute of Geology, Siberian Branch of Russian Academy of Sciences,
acad. Koptyug Av., 3. RU – 630090 Novosybirs’k, Russia
Amphiboles are important concentrators of REE in many types of magmatic
rocks. The published data was generalised on REE geochemistry in amphiboles
from some effusive rocks, mafic and ultramafic plutonic rocks (the total of about 100 analyses).
REE accumulation peculiarities in the mineral are considered the character of
their distribution spectra, the data on REE distribution indices in such
systems as amphibole/melt, amphibole/clinopyroxene, amphibole/plagioclase, and
the possible isomorphism mechanisms.
Ñ. 107–108
TYPOMORPHIC
PECULIARITIES OF THE GARNETS FROM METAMORPHIC ROCKS WITHIN RAKHIV ORE FIELD
V. Stepanov,
S. Kryzhevych
Ivan Franko National University of Lviv, Hrushevskogo
st. 4, UA – 79005 Lviv, Ukraine
Å-mail: geomin@geof.franko.lviv.ua
Physic-chemical peculiarities
of the garnets from metamorphic rocks within Rakhiv ore field have been
studied. These garnets as was ascertained belong to the rocks of the
greenschist metamorphism facies.
Key
words: garnets, quartz-micaceous slates, chemical composition, physical peculiarities,
metamorphism.
Ñ. 109–114
Paramagnetic centres in
zoned quartz from Volyn’ chamber pegmatites as indicators of its genesis
D. Voznyak1, V. Pavlyshyn2, A. Kalinichenko1, M.
Bagmut1
1Institute
of Geochemistry, Mineralogy and Ore Formation of NASU, Palladin Av., 34. UA-03680 Kyiv, Ukraine
The impure
and vacant paramagnetic centres in quartz from Volyn pegmatites have been
studied. It was shown that the concentration of the aluminium and germanium
centres decreases, and the number of the Å-centres increases, when the
polymorphic transformation of the high-temperature quartz in low-temperature one
occurs.
Key
words: quartz, growth zones, honeycomb quartz, paramagnetic centres,
temperature and γ-activation, pH and PT-parameters
of mineral-forming fluid.
Ñ. 115–120
DOVERITE AND ASSOCIATED Y-TR-CONTAINING MINERALS FROM RARE-METAL GRANITOIDS
PR2 OF PRIAZOVIAN REGION
N. Yashchenko
Crimean Branch of UkrSGRI, Kirov Av., 47/2, UA – 95017
Simferopol’, Ukraine
E-mail: imr@utel.net.ua
Y-TR-mineralization
(doverite, Y-bastnesite, synchisite, bastnesite, yttrofluorite, yttroapatite,
xenotime, monazite, fergusonite, pyrochlore) has been studied in rare-metal
lithium-fluoric hypersolvus granites of an agpaitic type. The basic mass of
fluorcarbonates Y-TR was crystallised simultaneously with biotite,
yttrofluorite at temperatures, close to solidus of high-fluoric hyper-solvus
granite.
Key words: mineralogy, petrology, rare-metal
lithium-fluoric granitoids, rare-earth elements, doverite, Y-bastnesite, yttrofluorite,
yttroapatite, Priazovian region, Ukrainian Shield.
Ñ. 121–129
MAIN STRUCTURAL-SUBSTANTIAL AND GENETIC CHARACTERISTICS
OF THE POBUZ’KÀ ENDERBITE-GNEISSIC FORMATION OF THE UKRAINIAN SHIELD
V. Kyrylyuk1, O. ²nozemtsev2
1Research
Centre of Ukrainian Ministry of Education and Science, Stepana Bandery St. 12, UA – 79013
Lviv, Ukraine
E-mail: kirvic@lviv.gu.net
2Complex
ecologic-geological party DP “Westukrgeology”',Zelena St. 111, UA – 79035
Lviv, Ukraine
E-mail: inozem@go.ru
The
regularities of the structure, petrochemical characteristics and geological
position of Early-Archean enderbite-gneisses supercrustal formation of the
granulite complex of the western part of the Ukrainian Shield are investigated. The data support the most probably primary
volcanic nature of the formation.
Key words:
Ukrainian shield, granulitic metamorphic complex, supercrustal formation,
hypersthene-bearing gneisses, crystalline schists, marbles, calciphyres, volcanic
nature.
Ñ. 130–136
Role of biogenic factor in formation
of copper mineralization in the Carpathian flysch deposits
O. Kostyuk, A. Kostenko
The article
deals with the origin of copper deposits in Skybova zone of the Ukrainian
Carpathians. The main objects of investigation are variegated deposits of
Yamnens’ka suite; among them are clay deposits, sandstone and conglomerates.
The problem under discussion is the biogenic influence on the copper deposits
formation. This question has not been given enough attention. Our hypothesis is
that blood system of some Mollusc, which contains haemocyanin, is the server
for creation of new copper concentrations.
Key words: copper mineralization, genesis, variegated
horizons, haemocyanin, Yamnens’ka suite, flysch, Carpathians.
Ñ. 137–145
ABOUT FLUID INCLUSIONS IN TOPAZ OF CRETACEOUS SEDIMENTS
OF NORTH-WESTERN VOLYN’ AND THEIR GENETIC SIGNIFICANCE
I. Naumko, Yu. Beletska, V. Kalyuzhnyj, R.
Lemishko
Institute of
Geology and Geochemistry of Combustible Minerals, Naukova St. 3a, UA – 79053
Lviv, Ukraine
Å-mail: igggk@.ah.ipm.lviv.ua
The results of fluid inclusion
study in the topaz of sedimentary carbonate-terrigenous series of Cretaceous
system of Volyno-Podillya plate within north-western Polissya are presented. It
is shown that by the typomorphic features of fluid inclusions topaz of Upper
Albian layers can be compared with the previously studied topaz of modern
lacustrine and alluvial sediments. Topaz of Lower Senoman layers – with topaz
of chamber type granite pegmatites from the north-western part of Ukrainian
Shield. This fact can favour definition of difference of paleogeografic
conditions of Albian and Senoman stages on the break of Early and Late
Cretaceous periods in the region.
Key words: fluid inclusions, topaz, sedimentary
series, Cretaceous period, north-western Volyn’.
Ñ. 146–151
GENETIC TYPES OF FLUID INCLUSIONS IN
HALITE FROM THE SALT-BEARING FORMATIONS OF UKRAINE
Institute of
Geology & Geochemistry of Combustible Minerals, Naukova st. 3a, UA – 79053 Lviv, Ukraine
Å-mail: igggk@ah.ipm.lviv.ua
Study on fluid inclusions in
sedimentary forms of halite of the salt-bearing formations of Ukraine showed
the presence of various genetic types of the inclusions. The proper
identification of the genetic type is essential to resolve various problems
such as the reconstruction of the chemical composition of brines in ancient
basins and seawater chemistry as well as the physical-chemical conditions of
recrystallization of salt.
Key words: halite, fluid inclusions, ultramicrochemical
analysis, evaporite formations.
Ñ. 152–156
SPECIAL FEATURES OF THE DEVONIAN ROCK-SALT
MINERAL COMPOSITION IN A ZONE OF CONTACT WITH MAGMATIC ROCKS (DNIEPER-DONETS
DEPRESSION)
V. Shaidets’ka
Institute of Geology & Geochemistry of Combustible
Minerals,
Naukova
st. 3a, UA – 79053 Lviv, Ukraine Å-mail:
igggk@ah.ipm.lviv.ua
In the Fammennian rock salt
(Dnieper-Donets Depression) from a zone of contact with diabase among the solid
inclusions in halite alongside with typical for halogen deposits authigene
minerals (carbonate, anhydrite, quartz, pyrite) the accessory minerals have
been discovered: garnet, amphibole, prehnite, epidote, chlorite. The
composition and typomorphic peculiarities of mineral impurities in halite are
the indicators of metasomatic processes happened in salt-bearing deposits under
the influence of diabase intrusion and postmagmatic processes.
Key words: evaporite, halite, intrusion, diabase, inclusions,
mineral impurities.
Ñ. 157–162
ASTRAKHANITE TRANSFORMATION UNDER RAISED TEMPERATURE CONDITIONS
Ivan Franko National University of Lviv, Hrushevskogo st.
4, UA – 79005 Lviv, Ukraine
Å-mail: geomin@geof.franko.lviv.ua
On the base of X-ray analysis phase transformation of the astrakhanite
under temperatures about 100, 150, 200, 250, 300 and 400°Ñ has been investigated. Astrakhanite dehydratation as was ascertained
takes place about 100°Ñ
while under 200°Ñ it transforms into lőweite. At 250°Ñ lőweite destroying has place as well as its transformation into
vanthoffite and perhaps antivanthoffite. In the natural conditions astrakhanite
transformation takes place under some lower temperature on the late diagenesis
and katagenesis stages.
Key words: astrakhanite, temperature, phase transformation, lőweite,
vanthoffite.
Ñ. 163–176
MINERAL CONTENT OF UROLITES OF ADULT PATIENTS UPPER URINE TRACKS FROM SOME
EUROPEAN COUNTRIES (the second half of the 20th century)
F. Zuzuk
E-mail: zuzuk@old.univer.lutsk.ua
The analysis of mineral content
of urolites of 24 collections from 11 European countries, which comprises 37 831
samples, has been carried out.
Phosphate, oxalate, urate, cystine and xanthine stones are
differentiated. Phosphate, oxalate, urate and cystine monomineral formations
are found correspondingly in 5.4, 23.1, 8.3 and 0.5 % of the total amount of
34.6 % of all studied samples. Widespread associations among phosphate, oxalate
and urate concrements reach correspondingly as far as 7.7, 46.7 and 7.1 % of
the 62.2 % of all studied samples. Rare associations correspondingly come to
2.8, 2.5 and 3.6 % of the total of 5.4 % of the studied samples. Number of all
associations for corresponding mineral formations comes to 8.1, 46.8 and 10.1 %
of the studied samples. Overall number
of associations equals to 62.0 % of all studied samples from the 24
collections. Two- and three-component associations are the most widespread
ones; they were encountered in the 24 collections correspondingly 78 and 54
times.
Key
words: biominerology, phosphates, oxalates, urates, Europe.
Ñ. 177–182
Academician M.V. Belov – outstanding crystallographer
and crystallochemist of 20th
century (regarding the 20th anniversary of his death)
O. Matkovs’kyi
E-mail: geomin@geof.franko.lviv.ua
The most important
achievements of the academician M.V. Belov in crystallography and crystallochemistry,
his organising and pedagogical gift have been analysed. His scientific
connections with Ukraine have been noted.
Key words: M.V. Belov, structural mineralogy, the most
dense packing, crystallochemical model, crystallographic school.