Greenpower Energy Ltd. provided the update regarding Turesi assay results at the Morabisi Lithium/REE Project. The majority of Turesi grab sample assays have now been received with 36 grab samples remaining for analysis at MS Analytical, Vancouver. The latest results from Turesi continue to encourage the GPP/GSM joint venture with grab samples from TT17-08 and TT17-09 where LiO2 values as high as 2.21% LiO2 have been returned. Of the 79 grab samples reported 28 samples returned values >1.0% LiO2. Channel samples from Trench TT17-06 have been received and confirm a zone of albite/kaolinite. The regional geology in the Morabisi area comprises a dominant WNW ­ ESE trending pegmatite and diabase from Turesi through to Banakaru. However, locally at Turesi there is an abundance of narrower Li-rich pegmatite dykes with a N-S orientation. These pegmatites occur over a minimum width of 500m (open to east) and in length they are open to the north and south. As more data becomes available geological features start to become evident. When looking at the Scintillometer data at Turesi there appears to be a strong N-S trending boundary where values suddenly decrease to the east, in total count intensity, within trenches TT17-05 and TT17-09. This is also evident in the analytical results recently received from Trench TT17-09. The LiO2 analytical values are of higher grade to the east of the boundary, mid-way through TT17-09. The scintillometer and assay values corelate well towards the east for approximately 500m (the extent of current analysed samples). In this 500m zone over 70 samples returned values >1.0% LiO2 and as high as 2.63% LiO2. Sampling extends 350m to the east with analyses still pending. To the west of this boundary the amount of spodumene identified is significantly less and the pegmatite is strongly kaolinized. Trench mapping indicates albite/kaolinite zones 400m from the boundary and identified in the western extent of Trench TT17-06. The boundary seen in the geology and the growing data set suggests LCT Pegmatite zonation of a larger WNW-ESE trending pegmatite. To the west of the boundary there is a kaolinized albite dominant zone and to the east, a Li-rich core or core margin zone. As more data is acquired, the understanding of the lithium mineralization increases.