Mineralization

The molybdenite mineralization is hosted in an 800 m long skarn zone composed of clinopyroxene, crystalline limestone (marble), limestone (skarn) and dolomite. Widths of skarn with MoS2 are up to 80 m wide and extend 500 m to depth. Molybdenite occurs as "veins" in fractures within the skarn and can become intensely clustered where molybdenite is greater than 20% in confined areas of 1m-2m widths. Molybdenite occurs as disseminated flakes throughout the skarn and is common in "banded" skarn.





Exploration

- December 16, 2011: NMC Resource Files Moland Molybdenum Technical Report
- November 1, 2011: NMC Resource Substantially Increases Mineral Resources At High Grade Producing Moland Mine
- October 4, 2011: NMC Resource Intersects High-Grade Molybdenum and Extends Deposit 40 Metres West
- September 27, 2011: NMC Resource Announces Additional High Grade Molybdenum Results Highlights
- August 23, 2011: NMC Resource Announces very High Grade Assay Results
- July 28, 2011: NMC Reports Increase in Molybdenum Value at NMC Moland Mine