Mt. Philips

Summary
The two tenements, E09/1337 & E09/1338, currently owned by Dynasty Metals are located in the Gascoyne region, WA. This project covers geological environments
with potential for Primary Uranium Deposits and Surficial Uranium in Calcrete sourced from the Proterozoic Granites of the Gascoyne province.

Geology:
The area is located on the southern side of a major faulted boundary between Durlachar & Morarie supersuites and Pooranoo & Morrisey Metamorphics Supergroup within the southern part of Palaeoproterozoic Gascoyne complex. The boundary is marked by a series of WNW trending faults and shear zones.

The Mt Phillips project is underlain by Archaean migmatities and Palaeoproterozoic schists and gneisses. These units have subsequently been intruded by mid Proterozoic granitoids and pegmatites, from partial melting of the Archean. During this period widespread deformation and retrograde metamorphism occurred, resulting in the formation of lower amphibolite to upper greenschist facies rocks.

There is a small inlier of Bangemall Basin continental and marine sediments unconformably overlying the Morrisey Metamorphics. The inlier is located on a strong WNW structural zone which may be a source of fluids.

Mineralisation
There are several mineralization styles in the region including calcrete hosted uranium, metamorphic uranium along with gold and base metal mineralisation. Pegmatite zones ~7km southwest of the tenement host uranium along with semi-precious stones, tantalumand lithium.

Figure 1. - The radiomentric image shows some anomalies in the North of tenement
E09/1337 and high variation in E09/1338.