Lanthanein Resources Ltd. announced that two surveys in preparation for the upcoming exploration programs at the Lyons Rare Earths Project in Western Australia (Lyons Project) are now complete. The proposed drill programs will target new highgrade ironstones similar to those previously drilled at Lyons 11, 12, 13 and 27. Further rock chip sampling, ground magnetics, high resolution satellite spectral interpretation and drilling programs are planned to investigate additional targets not yet followed up, including thorium and magnetic anomalies throughout the Lyons Project and the high priority structural target along the major Bald Hill lineament which transects both the Edmund and Lyons Project Areas.

The Bald Hill lineament is the major control on rare earth mineralisation at Hastings Technology Metals Yangibana mine and represents a very high priority target for Lanthanein. Potential remains for further discoveries of ironstones and carbonatites within the Company's tenure where no historical REE exploration has occurred. The Company recently received approval for $200,000 in cofunding from the Department of Mines Industry Regulation and Safety (DMIRS) for two deeper diamond holes (LI01_01 & LI03_01) to investigate potential for large tonnage REE carbonatites similar to Lynas Corporation's Mount Weld deposit in Western Australia.

Carbonatites are becoming increasingly important due to potential to host economic quantities of Th, U, Nb, P, Y and rare earth elements, which are strategically important for modern technology. Within the Lyons Block and along the Bald Hill Lineament, numerous carbonatite intrusions have been modelled from the airborne magnetics with a similar dimension to the Mt. Weld carbonatite.

Two drill holes to 450m depth are proposed the test the outer magnetic rim of two of the larger carbonatite intrusives including LI03 at 3km diameter and LI01 at 4km diameter. Fenitic alteration (incl. magnetite and Th) are found to be associated with the outer rim of these intrusive bodies.

A hybrid crosssectional model shows the outer magnetite halo from an initial carbonatite intrusive that continually exsolves fluids, building up Nb and REE in the outer magnetic and Sodic fenites. These modelled geophysical magnetic `crowns' or `cylinders' are interpreted to represent a similar carbonatite model. These outer fenite aureoles will be drill tested next month for Niobium (Nb) and rare earths (REE) which have initially developed from inner source alkaline silicate intrusives.