Convective modelling based on geophysical imaging of deep crustal intrusions - A new foundation for mineral exploration?

Cathles, L. M.; Cherkasov, S. V.; Vishnevskaya, N. A.

Global Tectonics and Metallogeny Volume 8 Number 1-4 (2003), p. 137 - 139

3 Literaturangaben

veröffentlicht: Jan 1, 2003

BibTeX Datei

ArtNo. ESP136000800046, Preis: 19.00 €

Vorschau PDF herunterladen Als PDF kaufen


The 200 x 500 km Yenisei Ridge metallogenic province, which runs along the southern reach of the north-flowing Yenesei River, is one of the great metallogenic provinces of the world. Pb, In, Au, Pt, Pd, Mn, and V ore occurrences are believed to have been produced, mainly by hydrothermal activity during a protracted period of rifting in Riphean time (1600-650 million years before present). Over 60 stratiform Pb-Zn deposits in carbonate and carbonate-ferruginous flysch occur in the western part of the Ridge, and over 20 major gold deposits in its eastern part.


geophysicalyenisei ridgehydrothermal activity