Abstract
The research problem of substituting existing hypotheses by a well-defined re modeling of the geological processes, which, in its turn, initiate and govern the formation of hydrothermal gold-ore deposits, is becoming more and more relevant. The four existing hypotheses - granitogene, basaltogene (magmagene), metamorphogene, and polygene have been considered and discussed. The interpretation of different hypotheses and analysis of substantiating facts showed the inconsistency of above-mentioned hypothesis-approaches. Up-dated petrological, petrochemical, geochemical data proved the following: generation of metal-bearing fluids in sources of moderate alkali-basalt melts during the late basalt formation stages show recycling Late Riphean to Late Paleozoic convergent antidromic granite diorite dolerite magmatic complexes.
| Original language | English |
|---|---|
| Article number | 012024 |
| Journal | IOP Conference Series: Earth and Environmental Science |
| Volume | 24 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 2015 |
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ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)
Cite this
Metallogenic problems of hydrothermal gold deposit formation : Facts and arguments. / Kucherenko, I. V.; Yuxuan, Zhang.
In: IOP Conference Series: Earth and Environmental Science, Vol. 24, No. 1, 012024, 2015.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Metallogenic problems of hydrothermal gold deposit formation
T2 - Facts and arguments
AU - Kucherenko, I. V.
AU - Yuxuan, Zhang
PY - 2015
Y1 - 2015
N2 - The research problem of substituting existing hypotheses by a well-defined re modeling of the geological processes, which, in its turn, initiate and govern the formation of hydrothermal gold-ore deposits, is becoming more and more relevant. The four existing hypotheses - granitogene, basaltogene (magmagene), metamorphogene, and polygene have been considered and discussed. The interpretation of different hypotheses and analysis of substantiating facts showed the inconsistency of above-mentioned hypothesis-approaches. Up-dated petrological, petrochemical, geochemical data proved the following: generation of metal-bearing fluids in sources of moderate alkali-basalt melts during the late basalt formation stages show recycling Late Riphean to Late Paleozoic convergent antidromic granite diorite dolerite magmatic complexes.
AB - The research problem of substituting existing hypotheses by a well-defined re modeling of the geological processes, which, in its turn, initiate and govern the formation of hydrothermal gold-ore deposits, is becoming more and more relevant. The four existing hypotheses - granitogene, basaltogene (magmagene), metamorphogene, and polygene have been considered and discussed. The interpretation of different hypotheses and analysis of substantiating facts showed the inconsistency of above-mentioned hypothesis-approaches. Up-dated petrological, petrochemical, geochemical data proved the following: generation of metal-bearing fluids in sources of moderate alkali-basalt melts during the late basalt formation stages show recycling Late Riphean to Late Paleozoic convergent antidromic granite diorite dolerite magmatic complexes.
UR - http://www.scopus.com/inward/record.url?scp=84923255562&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84923255562&partnerID=8YFLogxK
U2 - 10.1088/1755-1315/24/1/012024
DO - 10.1088/1755-1315/24/1/012024
M3 - Article
AN - SCOPUS:84923255562
VL - 24
JO - IOP Conference Series: Earth and Environmental Science
JF - IOP Conference Series: Earth and Environmental Science
SN - 1755-1307
IS - 1
M1 - 012024
ER -