Abstract
In the course of joint geologic-metallogenic investigations in the Northern Taymyr region, the distribution of gold was studied in the exocontact halos of the Upper Paleozoic plutons of the Lodochnikov complex. developed in the Northeast Taymyr region, which was carried out approximately on the abundance-ratio background level, established that the average gold content, as determined from 233 samples by the neutron-activation and polarographic methods, is 3.17 ppb. The trends of behavior of gold established at about the abundance-ratio level is also confirmed by analysis of higher concentration of it, associated with hydro-thermal-metasomatic rocks developed around the granitoid intrusive; zones of pyrite-pyrrhotite impregnation, quartz and quartz-sulfide veinlets, argillization, etc. Thus we have confirmed the possibility in principle that ore lodes can be formed by the redistribution of gold through the action of contact metamorphism, which essentially, reflects a single mechanism that is realized also in regional zonal metamorphism.
| Original language | English |
|---|---|
| Pages (from-to) | 295-297 |
| Number of pages | 3 |
| Journal | Doklady. Earth science sections |
| Volume | 313 |
| Issue number | 4 |
| Publication status | Published - Jul 1990 |
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Geochemical model of the gold distribution in the exocontact halo of a granitoid mass. / Zabiyaka, A. I.; Vernikovskiv, V. A.; Zabiyaka, I. D.; Zlobin, M. N.; Korobeynikov, A. F.; Serdyuk, S. S.
In: Doklady. Earth science sections, Vol. 313, No. 4, 07.1990, p. 295-297.Research output: Contribution to journal › Article
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TY - JOUR
T1 - Geochemical model of the gold distribution in the exocontact halo of a granitoid mass
AU - Zabiyaka, A. I.
AU - Vernikovskiv, V. A.
AU - Zabiyaka, I. D.
AU - Zlobin, M. N.
AU - Korobeynikov, A. F.
AU - Serdyuk, S. S.
PY - 1990/7
Y1 - 1990/7
N2 - In the course of joint geologic-metallogenic investigations in the Northern Taymyr region, the distribution of gold was studied in the exocontact halos of the Upper Paleozoic plutons of the Lodochnikov complex. developed in the Northeast Taymyr region, which was carried out approximately on the abundance-ratio background level, established that the average gold content, as determined from 233 samples by the neutron-activation and polarographic methods, is 3.17 ppb. The trends of behavior of gold established at about the abundance-ratio level is also confirmed by analysis of higher concentration of it, associated with hydro-thermal-metasomatic rocks developed around the granitoid intrusive; zones of pyrite-pyrrhotite impregnation, quartz and quartz-sulfide veinlets, argillization, etc. Thus we have confirmed the possibility in principle that ore lodes can be formed by the redistribution of gold through the action of contact metamorphism, which essentially, reflects a single mechanism that is realized also in regional zonal metamorphism.
AB - In the course of joint geologic-metallogenic investigations in the Northern Taymyr region, the distribution of gold was studied in the exocontact halos of the Upper Paleozoic plutons of the Lodochnikov complex. developed in the Northeast Taymyr region, which was carried out approximately on the abundance-ratio background level, established that the average gold content, as determined from 233 samples by the neutron-activation and polarographic methods, is 3.17 ppb. The trends of behavior of gold established at about the abundance-ratio level is also confirmed by analysis of higher concentration of it, associated with hydro-thermal-metasomatic rocks developed around the granitoid intrusive; zones of pyrite-pyrrhotite impregnation, quartz and quartz-sulfide veinlets, argillization, etc. Thus we have confirmed the possibility in principle that ore lodes can be formed by the redistribution of gold through the action of contact metamorphism, which essentially, reflects a single mechanism that is realized also in regional zonal metamorphism.
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UR - http://www.scopus.com/inward/citedby.url?scp=0025449802&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:0025449802
VL - 313
SP - 295
EP - 297
JO - Doklady. Earth science sections
JF - Doklady. Earth science sections
SN - 0012-494X
IS - 4
ER -