Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Ye. M. Shmariovich"'
Publikováno v:
International Geology Review. 32:734-745
(1990). PHYSICOCHEMICAL EXPLANATION OF THE PHASE-BY-PHASE NATURE OF THE HYDROTHERMAL URANIUM-ORE PROCESS. International Geology Review: Vol. 32, No. 7, pp. 734-745.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6465f919e2b32ccb52e2b03972774789
https://doi.org/10.1080/00206819009465814
https://doi.org/10.1080/00206819009465814
Publikováno v:
International Geology Review. 32:517-522
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::20f2d39abab60206ed4691b0d17be0f3
https://doi.org/10.1080/00206819009465795
https://doi.org/10.1080/00206819009465795
Publikováno v:
International Geology Review. 31:424-430
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f07bae008f21f259d148470e34b5c66a
https://doi.org/10.1080/00206818909465895
https://doi.org/10.1080/00206818909465895
Publikováno v:
International Geology Review. 26:197-205
Halos of hematitization generally occur in the peripheral, more dense areas surrounding impregnated pitchblende ores, in rocks surrounding veinlets of pitchblende and in the gouge of these veinlets. The breadth of the reddening halo in the rocks can
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::44c1ffb5b1618c0c748be97852cb4a60
https://doi.org/10.1080/00206818409466548
https://doi.org/10.1080/00206818409466548
Autor:
Ye. M. Shmariovich
Publikováno v:
International Geology Review. 24:1174-1182
Uranyl minerals form a distinct series based on their solubilities in environments of different pH, beginning with the molybdenates, and proceeding through the arsenates, phosphates, vanadates, and silicates of the soddyite groups. Unlike exogenetic-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e08807288c728d67c39b1a638c7202dc
https://doi.org/10.1080/00206818209451056
https://doi.org/10.1080/00206818209451056
Publikováno v:
International Geology Review. 29:491-498
Previous experiments have characterized the behavior of uranium in sulfide-carbonate solutions at 200/sup 0/C, analogous to the solutions that produced many endogenous pitchblende deposits, as indicated by fluid inclusions in minerals and by mineralo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b8ce08569b0e5e56fc8bdc9ed8527ad0
https://doi.org/10.1080/00206818709466166
https://doi.org/10.1080/00206818709466166
Publikováno v:
International Geology Review. 28:461-470
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7f6e8c770598f466fc21b9553ee989ff
https://doi.org/10.1080/00206818609466286
https://doi.org/10.1080/00206818609466286
Publikováno v:
International Geology Review. 16:600-609
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2517bc860bb1c45747456e7549430d80
https://doi.org/10.1080/00206817409471843
https://doi.org/10.1080/00206817409471843
Autor:
Ye. M. Shmariovich, M. F. Maksimova
Publikováno v:
International Geology Review. 25:189-195
The distribution of rhenium in the profile of an ore-controlling zonation in complex exogenic, uranium-coal deposits is described. It is established that the earlier suggested distinct association between rhenium and molybdenum is lacking in the ores
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::812ba649870b8d33c332d14333776648
https://doi.org/10.1080/00206818309466691
https://doi.org/10.1080/00206818309466691
Autor:
Ye. M. Shmariovich, I. S. Modnikov
Publikováno v:
International Geology Review. 31:79-89
(1989). THE PROBLEM OF THE SOURCE OF THE URANIUM OF URANIUM ORE DEPOSITS. International Geology Review: Vol. 31, No. 1, pp. 79-89.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4351101a81fec9416d75264b42b84f1
https://doi.org/10.1080/00206818909465863
https://doi.org/10.1080/00206818909465863