Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Maxim O. Vityk"'
Publikováno v:
Contributions to Mineralogy and Petrology. 139:285-297
The nature and abundance of dislocations in quartz surrounding fluid inclusions were studied to obtain a better understanding of processes associated with fluid inclusion reequilibration. Synthetic fluid inclusions containing 10 wt% NaCl aqueous solu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c9434128ade07c150eb17c72d6bb7763
https://doi.org/10.1007/s004100000142
https://doi.org/10.1007/s004100000142
Autor:
Maxim O. Vityk, Robert J. Bodnar
Publikováno v:
Contributions to Mineralogy and Petrology. 132:149-162
Fluid inclusion microthermometric data are often reported as homogenization temperature frequency histograms. Interpretation of such histograms for a single fluid inclusion assemblage (FIA) of non-reequilibrated fluid inclusions is usually straightfo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::74585dbcd32cb829fbca99a1b98e15e6
https://doi.org/10.1007/s004100050413
https://doi.org/10.1007/s004100050413
Publikováno v:
Tectonophysics. 255:163-174
Fissures in the nappes of the Folded Carpathians contain euhedral quartz crystals known as Marmarosh Diamonds. Study of Marmarosh Diamonds collected from the nappes in the Ukrainian part of the Carpathians showed that these quartz crystals contain ab
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::49fe39acc0da2691e38ffab4d27f1362
https://doi.org/10.1016/0040-1951(95)00128-x
https://doi.org/10.1016/0040-1951(95)00128-x
Publikováno v:
European Journal of Mineralogy. 7:1071-1088
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f8801da6c5df2fef76b08b36c69a89b8
https://doi.org/10.1127/ejm/7/5/1071
https://doi.org/10.1127/ejm/7/5/1071
Autor:
Maxim O. Vityk, Robert J. Bodnar
Publikováno v:
Contributions to Mineralogy and Petrology. 121:309-323
Experimental reequilibration of synthetic 10 wt% NaCl-H2O inclusions in natural quartz reveals that reequilibration textures show distinct differences depending upon the P-T path followed by the inclusion after formation. These differences combined w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3e14fd4b9c869d8be1bfc3176cbd67f7
https://doi.org/10.1007/bf02688246
https://doi.org/10.1007/bf02688246
Publikováno v:
Economic Geology. 89:547-565
The Beregovo vein-type gold-base metal deposit is hosted by volcanic sedimentary sequences of the Pannonian basin in the Carpathian Neogene volcanic belt. Four stages of mineralization were distinguished: (1) sulfide, (2) quartz-barite, (3) carbonate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::35fe1249063fddf9dfff4ec394e2a826
https://doi.org/10.2113/gsecongeo.89.3.547
https://doi.org/10.2113/gsecongeo.89.3.547
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