Member Info for bbr391

Could be friends with Pablo Escobar .

Best of Luck All On the Path

Best of Luck All On the Path

11 April 2017 � Independent Power Corporation PLC (IPC) is proud to announce the establishment of a new power development company, QG Power Africa (QGPA). This joint venture, with engineering consultancy Tom� International and the US$250 million Quantum Global Mezzanine Fund, has been set up to develop power plants across countries in the sub-Saharan Africa region. It will focus, during its initial phase, on Angola, Botswana, Mozambique, Uganda, Nigeria, Kenya and Ghana. QGPA will expand its development capabilities to meet Africa�s fast growing demand for power.

http://www.indpow.co.uk/

And the fight for Restoration goes on . Best of Luck All On The Path

PE stinks. It`s Official Best of Luck All

Peter as usual starts with a damp squib . Let`s hope he turns a corner . But don`t hold your breath Ever the Optimist

Looks like PE has started already . Best of Luck All IPC value $250 million.

A move over 0.26 would be nice. Come on Mr Will I ams . Best of Luck All

Excellent value at today`s price. Although not too impressed by the BOD`s achievements thus far. One lives in hope Best of Luck All

Release of Transcript Restriction set for 11/1/2017. With luck the share price will rise nicely from here . Bottoms Up All

That is the six million dollar question. Let`s hope for a decent return ,somewhere above today`s NAV ..

Involved in lekoil sterling energy Chariot & others. More money philanderers / lenders

Peter will have Sterling in the bag already . We now fight over the other 20% + . Let`s hope we get a fair deal . Best of Luck All

Or less sellers Best of Luck All

scottcorp . One hopes the uptick will continue on further good news ,before the big event in november . Best of Luck

Zacatecas Lithium Brine Project - Mexico 11 shallow auger holes (15-27m deep) completed at San Juan Salar. Assay results show strong lithium in salt lake sediments up to 874ppm Li, confirming highly anomalous surface sample results; Near surface water samples are not strongly saline, perhaps due to rainwater dilution. However lithium and total salinity in brine samples increase with depth in all holes pointing to deeper target; MT geophysical survey planned to assess deeper brine targets prior to drill testing. ----------------------- Seems the BOD have not learnt from Zenith , that depth is the key . Disappointing . Best of Luck All

My hope is that this new regional play ,Involves good figures for Arian . One could envisage this under-performer hitting double figures MCAP wise . IF the results are Appropriately positive . We may see an extra purchase of acreage first ,whom knows . Good luck All

Zenith Zacatecas ; The Zacatecas brine targets are considered by the Company to be most similar to those hosted in the immature salt lake systems such as at Clayton Valley (host to the USA’s only lithium brine operation, Silver Peak in Nevada where the lithium brines aquifers are stratified and occur in specific aquifers towards the deeper portions of the host basins (Figure 2). Lithium brine projects can be subdivided into two broad deposit types, depending on the salt lake/salt basin (salar) characteristics (Houston et al., 2011): • Mature salars (those containing extensive thicknesses – often hundreds of meters - of halite (salt), such as those in the Argentina and Chile- the Salar de Atacama, and the FMC Hombre Muerto operation). These Mature salt dominated salars are characterized by having high permeability and specific yields (to a maximum of ~ 15 % Sy) near surface, with the porosity and permeability decreasing rapidly with depth. In these salars the brine resource is essentially between surface and 50 m below surface, as below this depth there is limited permeability in the salt, due to salt recrystallization and cementation of fractures; and • Immature salars, which are dominated by clastic sediments, with limited thicknesses of halite.-, such as those known at Clayton Valley in Nevada. and Zenith’s model for Zacatecas Immature salars conversely have porosity and permeability controlled by individual layers within the salar sequence. The porosity and permeability may continue to depths of hundreds of meters in clastic salars. A schematic cross section produced by the Servicio Geologico Mexicano (Figure 2a) located immediately west of Zenith’s San Juan Salar at Zacatecas, shows interpreted deep (to 400m) Tertiary Lake Sediments beneath a calcrete layer that may act as an aquaclude (water barrier), segregating ground water layers potentially of different salinity and composition. A comparative schematic section of the Clayton Valley basin is shown in Figure 2b at the same scale to highlight similarities in the model, illustrating the near surface nature of the recent 15-27m deep auger holes at San Juan Salar.