Abstract
NAA of Au in a number of minerals from different intrusive and skarn rocks enables calculation of a coefficient of accumulation (Ka) which indicates a persistent accumulation of metal in all intrusive rocks studied (Ka 1.3-3.5) in the fine-grained rock matrix. Higher Au concentrations in minerals of pegmatites and contact-metasomatites (Ka 20-190) indicate substantial Au accumulation. Experimental data indicate the ratio of partition of Au between fluid phase and ore-generating granitic melt is approx 50. -S.R.
| Original language | English |
|---|---|
| Title of host publication | Doklady, Academy of Sciences of the USSR, Earth Sciences Section |
| Pages | 193-196 |
| Number of pages | 4 |
| Volume | 258 |
| Publication status | Published - 1983 |
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ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)
Cite this
Gold fractionation in crystallizing magma. / Korobeynikov, A. F.
Doklady, Academy of Sciences of the USSR, Earth Sciences Section. Vol. 258 1983. p. 193-196.Research output: Chapter in Book/Report/Conference proceeding › Chapter
}
TY - CHAP
T1 - Gold fractionation in crystallizing magma.
AU - Korobeynikov, A. F.
PY - 1983
Y1 - 1983
N2 - NAA of Au in a number of minerals from different intrusive and skarn rocks enables calculation of a coefficient of accumulation (Ka) which indicates a persistent accumulation of metal in all intrusive rocks studied (Ka 1.3-3.5) in the fine-grained rock matrix. Higher Au concentrations in minerals of pegmatites and contact-metasomatites (Ka 20-190) indicate substantial Au accumulation. Experimental data indicate the ratio of partition of Au between fluid phase and ore-generating granitic melt is approx 50. -S.R.
AB - NAA of Au in a number of minerals from different intrusive and skarn rocks enables calculation of a coefficient of accumulation (Ka) which indicates a persistent accumulation of metal in all intrusive rocks studied (Ka 1.3-3.5) in the fine-grained rock matrix. Higher Au concentrations in minerals of pegmatites and contact-metasomatites (Ka 20-190) indicate substantial Au accumulation. Experimental data indicate the ratio of partition of Au between fluid phase and ore-generating granitic melt is approx 50. -S.R.
UR - http://www.scopus.com/inward/record.url?scp=0021061139&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0021061139&partnerID=8YFLogxK
M3 - Chapter
VL - 258
SP - 193
EP - 196
BT - Doklady, Academy of Sciences of the USSR, Earth Sciences Section
ER -