期刊缩写       ANN SOC GEOL POL

期刊全称       ANNALES SOCIETATIS GEOLOGORUM POLONIAE

期刊ISSN      0208-9068

2013-2014最新影响因子     0.727

期刊官方网站       http://www.asgp.pl/74_3_267

期刊投稿网址      

通讯方式       POLISH GEOLOGICAL SOC, UL. OLEANDRY 2A, KRAKOW, POLAND, 30-063

涉及的研究方向    地学-地质学

出版国家       POLAND

出版周期       Quarterly

出版年份       0

年文章数       24

PubMed Central (PMC)链接 http://www.ncbi.nlm.nih.gov/nlmcatalog?term=0208-9068%5BISSN%5D

平均审稿速度（网友分享经验）       >12周，或约稿

平均录用比例（网友分享经验）       容易

 

 

Annales Societatis Geologorum Poloniae (ASGP) is a scientific journal of the Geological Society of Poland. Original contributions, review papers and book reviews from all branches of geological sciences, including applied and economic geology, as well as discussions to the papers previously published in this journal are considered for publication in Annales Societatis Geologorum Poloniae. The language of the journal is English.

 

ASGP (2004), vol. 74: 267-276

 

ORIGIN OF THE BADENIAN SALTS FROM EAST SLOVAKIAN BASIN INDICATED BY THE ANALYSIS OF FLUID INCLUSIONS

 

Anatoliy R. GALAMAY (1), Krzysztof BUKOWSKI (2), Andriy V. POBEREZHSKYY (1), Stanislav KAROLI (3) & Volodymyr M. KOVALEVYCH (1)

 

1) Institute of Geology and Geochemistry of Combustible Minerals, National Academy of Sciences of Ukraine, Naukova 3A, 79053 Lviv, Ukraine, igggk@ah.ipm.lviv.ua

2) Faculty of Geology, Geophysics and Environment Protection, University of Science and Technologyy, Mickiewicza 30, 30-059 Kraków, Poland, buk@geolog.geol.agh.edu.pl

3) Geological Survey of Slovak Republic, Werferova 1, 04011 Ko?ice 1, Slovakia, karoli@gssr-ke.sk

 

Galamay, A. R., Bukowski, K., Poberezhskyy, A. V., Karoli, S. & Kovalevych, V. M., 2004. Origin of the Badenian salts from East Slovakian basin indicated by the analysis of fluid inclusions. Annales Societatis Geologorum Poloniae, 74: 267-276.

 

Abstract: Chemical composition of the brines of primary fluid inclusions in sedimentary halite (from the boreholes: P-2, P-3, P-6, P-7 and P-8) of the Badenian evaporite of the Zbudza Fm. from East Slovakian basin indicates that the basinal brines belong to the Na-K-Mg-Cl-SO4 type. The ratios of K+, Mg2+, and SO42- ions are practically the same as they were in the Badenian seawater.

 

Taking into account the information on the chemical evolution of seawater in the Phanerozoic (Kovalevich et al., 1998) and the calculations of this evolution for the Cenozoic (Zimmermann, 2000) it is suggested that the Badenian seawater was characterized by the reduced contents of Mg (by approximately 20%) and SO42- (by approximately 40%) in comparison with the recent seawater.

 

The postsedimentary recrystallization of salts occurred under the effect of buried brines, which inherited their composition from the primary basinal brines. The intensive recrystallization of salts occurred during the tectonic movements.