International scientific-practical conference - „The Development of Mining and Geology is the Precondition for the Revival of Economy”
On September 23-24, 2021 Mineralogical Society of Georgia, G. Tsulukidze Mining Insitute and Georgian Technical University will hold International Scientific-Practical Conference - „The Development of Mining and Geology is the Precondition for the Revival of Economy”
Conference Venue:
Sep 23 - Georgian Technical University
77 Kostava st., Administrative Building, Georgian Technical University, 0160, Tbilisi.
Sep 24 - RMG GOLD
Kazreti, Bolnisi Municipality
The abstracts should be sent to e-mail: msgeorgia2012@gmail.com
For additional information see the web-site: www.msgeorgia2012.com
Contact persons:
Maia Kobaxidze Tel: (+995) 599 91-67-68 |
Asmat Shekiladze Tel: (+995) 599 70-84-28 |
Ketevan Gabarashvili Tel: (+995) 593 31 73 97 |
Guidelines for abstracts
1 - The abstract should be represented in English; appropriate Georgian or Russian versions must be attached;
2 - The abstract should not exceed two pages;
3 - The abstract should be done in the following form:
The co-authors from different institutions should be marked with superscript (see the pattern);
4 - Each author may submit not more than two abstracts;
5 - The abstracts are to be sent to – msgeorgia2012@gmail.com
6 - The deadline for the abstract submission is APRIL 30, 2021;
7- The abstracts, not fitted with the requirements, will not be accepted;
8 - Poster presentation - size – 100 × 80 cm. The deadline for the poster el. version submission is
May 10, 2021.
Editorial board
Pattern:
MINERALOGICAL FEATURES OF CHALCEDONY-AGATE FROM
AKHALTSIKHE FIELD
THE FIRST AUTHOR1, THE SECOND AUTHOR2
1Georgian Technical University, Tbilisi, Georgia
2A. Janelidze Institute of Geology of Tbilisi State University, Tbilisi, Georgia
According to the data of the researches of the chalcedony-agate samples from the Akhaltsikhe deposit carried out by optical-microscopic, X-ray phase, and X-ray fluorescence methods and the data existing in technical literature, it has been concluded that certain geode layers, often characterized by alternation of variously colored bands with concentric-zonal formations, are represented by various phases……..
Table 1
Composition of intrusive rocks (№11, bold)
№ |
SiO2 |
TiO2 |
Al2O3 |
Fe2O3 |
FeO |
MnO |
CaO |
MgO |
P2O5 |
Na2O |
K2O |
H2O+ |
1 |
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2 |
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3 |
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4 |
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REFERENCES
Benidze G. The Peculiarities of Organic Carbon Distribution and Postdiagenetic Transformations in the Lower and mid- Jurassic Shale Terrigenic Sediments of Beyond-Alazani, Kakheti. Caucas. Inst. Min. Res., 2009, pp. 170-178 (in Georgian).