Post by pling on Feb 10, 2016 19:49:55 GMT
Fra nordicmining 10. februar 2016
Estimation of Mineral Resources at Nesodden hydrothermal Quartz deposit Southwest Norway
- Due to good continuity of the quartz vein complex system as seen in the detailed surface mapping and a good continuity in the vertical direction between the drillholes and the surface mapping, a certain amount of the estimated hydrothermal quartz content are classified as indicated resources. This is defined by not being to distal to the drillholes. The part that is being regarded as too distal from the drillholes, but still appears to have good continuity regarding the surface mapping, is then estimated as inferred resources. The part of the quartz vein complex between the southwestern and the northeastern parts that appears to be rather disturbed and deformed and possibly contains a shallow dipping shear zone (discussed in the geology chapter), has not been estimated. Even though that part of the hydrothermal quartz vein system is definitely occurring according to the surface mapping.
Quartz Resource:
Indicated: 2,9 mill. tonn @ 65%
Inferred: 1,35 mill. tonn @ 66%
Indicated + inferred: 4,25 mill. tonn @ 65%
Hydrothermal Quartz:
Indicated: 1,9 mill. tonn
Inferred: 0,9 mill. tonn
Indicated + inferred: 2,8 mill. tonn
+ "...the quartz vein between the southwestern and the northeastern parts has not been estimated".
Estimation of Mineral Resources at Nesodden hydrothermal Quartz deposit Southwest Norway
- Due to good continuity of the quartz vein complex system as seen in the detailed surface mapping and a good continuity in the vertical direction between the drillholes and the surface mapping, a certain amount of the estimated hydrothermal quartz content are classified as indicated resources. This is defined by not being to distal to the drillholes. The part that is being regarded as too distal from the drillholes, but still appears to have good continuity regarding the surface mapping, is then estimated as inferred resources. The part of the quartz vein complex between the southwestern and the northeastern parts that appears to be rather disturbed and deformed and possibly contains a shallow dipping shear zone (discussed in the geology chapter), has not been estimated. Even though that part of the hydrothermal quartz vein system is definitely occurring according to the surface mapping.
Quartz Resource:
Indicated: 2,9 mill. tonn @ 65%
Inferred: 1,35 mill. tonn @ 66%
Indicated + inferred: 4,25 mill. tonn @ 65%
Hydrothermal Quartz:
Indicated: 1,9 mill. tonn
Inferred: 0,9 mill. tonn
Indicated + inferred: 2,8 mill. tonn
+ "...the quartz vein between the southwestern and the northeastern parts has not been estimated".