| Lat / long: | 69.30447, 88.28588 |
| Primary: | Copper, Nickel, Platinum |
| Orebody form: | CHONOLITHS, NORTH INTRUSION ELLIPSE IN CROSS-SECTION, LONG AXIS DIPS SE, INTRUSION RISES TO SOUTH. HANGING WALL IS STEEPER THAN FOOT WALL. SOUTH INTRUSION IS SIMILAR, BUT BRANCHES AND RISES TO THE NORTH |
| Operation type: | Unknown |
| Production size: | None |
| Development status: | Prospect |
| Host rock: | Marine Sediments;Shallow Marine Sediments;Tunguska Series, Continental And Lagoonal Sediments |
| Host type: | Diorite,Diabase,Basalt |
| Alteration processes: | One Of The More Altered Of The Nori*k Intrusions |
| MRDS | M045645 |
| DEP | 10038313 |
| Reference | {Deposit:: MERTIE, J.B.,JR,1969, ECONOMIC GEOLOGY OF PLATINUM METALS, U.S.G.S. PROF. PAPER 630, P. 60-63.}{Deposit:: SMIRNOV, M.F., 1966, THE STRUCTURE OF NORI*K NICKEL-BEARING INTRUSIONS AND THE GENETIC TYPES OF THEIR SULPHIDE ORES. VSESOYUZNYI-NAUCHNO ISSLEDOVATE*KII INSTITUT MINERAL*OGO SYRIA} |
| Reporter | Page, Norman J., Till, Alison B. |