Skarn radiogeochemical features; Geochemistry International; Vol. 22, iss. 6

Opis bibliograficzny
Parent link:Geochemistry International.— , 1985
Vol. 22, iss. 6.— 1985.— P. 144-157
1. autor: Rikhvanov L. P. Leonid Petrovich
Kolejni autorzy: Sarnayev S. I., Bezkhodarnova T. E.
Streszczenie:Data are given on the behaviour of U and Th during skarn formation. The concentrations and forms of these elements in main skarn minerals are considered. The skarns in the region are characterized by an influx of U and reduction in the Th/U ratios. The elevated U concentrations were produced by infiltrating hydrothermal solutions.
В фонде НТБ ТПУ отсутствует
Język:angielski
Wydane: 1985
Hasła przedmiotowe:
Format: xMaterials Rozdział
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=595796

MARC

LEADER 00000naa0a2200000 4500
001 595796
005 20250317103918.0
035 |a (RuTPU)RU\TPU\tpu\17552 
035 |a RU\TPU\tpu\17073 
090 |a 595796 
100 |a 20100526d1985 k||y0rusy50 ba 
101 0 |a eng 
102 |a DE 
200 1 |a Skarn radiogeochemical features  |f L. P. Rikhvanov, S. I. Sarnayev, T. E. Bezkhodarnova 
330 |a Data are given on the behaviour of U and Th during skarn formation. The concentrations and forms of these elements in main skarn minerals are considered. The skarns in the region are characterized by an influx of U and reduction in the Th/U ratios. The elevated U concentrations were produced by infiltrating hydrothermal solutions. 
333 |a В фонде НТБ ТПУ отсутствует 
461 |t Geochemistry International  |d 1985 
463 |t Vol. 22, iss. 6  |v P. 144-157  |d 1985 
610 1 |a труды учёных ТПУ 
700 1 |a Rikhvanov  |b L. P.  |c Professor of Tomsk Polytechnic University  |c Doctor of geological- mineralogical sciences  |c Honored geologist of Russia  |c Honored employee of higher vocational education of the Russian Federation  |f 1945-  |g Leonid Petrovich  |3 (RuTPU)RU\TPU\pers\25922 
701 1 |a Sarnayev  |b S. I. 
701 1 |a Bezkhodarnova  |b T. E. 
801 1 |a RU  |b 63413507  |c 20100112 
801 2 |a RU  |b 63413507  |c 20140329  |g RCR 
942 |c CR