Ochre Hill EL 9999 Annual Report for the period 22 July 2011 to 21 July 2012

Abstract

Geological mapping over the Jasmine - North Beryl - Ochre Hill Area was carried out within the reporting period. EL 9999 forms part of this area. The iron mineralisation was found to occur as thin brecciated units within the Lower Wildman Formation. The iron breccia occupies the eastern limb of a major northwest plunging syncline. Mineralisation is interpreted to sit in a region of structural faulting where dilational jogs have allowed significant mineralisation to occur. The mapping was completed by taking notes while traversing the mapping area, and interpretations were made via aerial photography. A total of 23 rock-chip samples were collected during the reporting period (from this report and other field visits). During the reporting period Territory Resources obtained satellite imagery over the entirety of the Frances Creek Project. This satellite imagery was acquired from GeoImage, which also included ortho-rectification and digital surface modeling for contouring. The satellite imagery is in Appendix 3; this has been submitted on hard drive as the data is very large.