@BRProject - Allow me to add to this; the Dobra participation...

@BRProject - Allow me to add to this; the Dobra participation will be a huge plus to EUR. It is geologically ultra-rich in the desired metals and more and is located in the middle of the Ukraine and with some luck the area will not have sustained much war damage. At end of war - and we don't know how and when this will end, but end it will - there will have to be a concerted effort by the NATO nations to help with the rebuild, much like the Marshall Plan effected for Post-War Europe - and they will certainly be interested in mineral exploration to help pay for it all.
Now we are still waiting who will win this war!
I am too old to wait this out - but posters and holders on here stand to benefit, should this go ahead. I have copied this over from a Ukrainian Government site and some words may run into one another - I don't have the time to re-type - the bolding is mine.

DOBRA:

Location: Novoukrainskyi district of Kirovograd region.
Block area: 1707 ha.

Geological summary:

Geotectonically the object is located in the western part of the Kirovohrad mega block of the Ukrainian Shield within the Bratskyi composite syncline of the Early Proterozoic Era. Theprospective field is confined to the Mykhailivka tectonic-metasomatic zone, which is a component of the Zvenigorod-Hannivka fault zone and borders the western part of the Lipnyazkyi granite dome.

The Dobrablock is located within the Stankuvatsky ore field of the Central Ukrainian (Shpolyansko-Tashlytsky) rare metal district. Pegmatites, which make up the productive ore zones of both prospective fields, belong to thesodium-lithium type. The metallogenic trend of Stankuvatsky and Nadiya prospective areas is determined by lithium, tantalum, gold, and tungsten. Often ore mineralization of different elements is spatiallycombined, therefore the discovered prospective object is complex.

The Stankuvatsky prospective field combines the whole range of basic elements inherent in the Mykhailivska zone - lithium, tantalum, gold andtungsten. The spatial combination of lithium and tantalum ore formation is peculiar to Nadiya prospective field. The mineral of the block is represented by lithium ores podumen-petalite mineral composition (usefulcomponent - lithium). Productive ore zones of Nadiya and Stankuvatske prospective fields are vein zones of sodium-lithium pegmatites deposited in amphibole crystalline shales. The basement rocks are overlain byloose terrigenous deposits of the Meso-Cenozoic platform cover and weathering crust. The Stankuvatsky prospective field is traced for a stretch of 2 km by 6 profiles of deep wells. In its northern part it is studied by agrid of wells with a density of 350-200 x 200-100 m, in the central and southern part - 650-600x260-100 m. The host rocks are represented by amphibolites and gneisses.

Lithium ores are represented by rare metalpegmatites with petalite, spodumene, triphylline, less often hillmquistite and amblygonite. Petalite predominate among ore minerals. The average content of lithium oxide in ores is 1.30%. The amount of lithiumminerals in ores varies from 1-2% to 85%, on average 30-40%. The following types of ores are distinguished by the predominant lithium mineral: petalite - 32% of the total amount, spodumene - 28%, spodumene-petalite - 17% and petalite-spodumene - 23%. There are no patterns of different types placement. Mixed type prevails.

Petalite ores form areas of rocks with a trunk thickness of the first to tens of meters. Lithium isassociated with petalite (16-48.6%), spodumene (13.6-76%), and trifillin (3.2-8%). Lithium ores of prospective field are formed by three ore zones. Nadiya prospective field is traced for 2.1 km by 4 profiles of deepwells drilled on a grid of 800-680 x 200-130 m in the north and 370-310 x 250-100 m in the south of the ore occurrence. The productive stratum is 1,600 m in length, horizontal span 340-390 m. Lithium minerals arerepresented by spodumene, petalite, triphylline, less often by amblygonite and holmquistite. Predominant (?? typo!! should it be 'Petalite'?) is predominant. The average content of lithium oxide in ores is 1.31%.

Container rocks are also representedby amphibolites and gneisses. According to the complexity of the geological structure, the block of lithium ore: Dobra is classified as a deposit of complex geological structure (group 2) in accordance with theClassification of reserves and resources of minerals of the State fund of mineral reserves.

Mining and geological operating conditions are characterized by a steep fall and depth of ore deposits. Significant thickness ofoverburden (up to 80 m) determines the choice of underground method of field development.

Available geological information: Stankuvatskyi and Nadiya lithium ore were discovered by #47 expedition of Kirovgeologiya SE in 1989 during exploration at a scale of 1:50 000 for gold and liquid metals.

In1991-2001, during prospecting lithium and gold deposits at a scale of 1:25 000-1: 10 000. In 2017, by the decision of the State Commission on Mineral Reserves of Ukraine (#4142 protocol as of November 1, 2017), theNadiya and Stankuvatske ore were united into one ore zone - Dobra block.

Fund materials:
1. Inv. #58673 "Results of prospecting of lithium and gold deposits at a scale of 1: 25000-1: 10000 framed by the Lipnyazhskyi granite dome on the area of 100 m2 with an assessment of the revealed prospective fieldand resources of P1 and P2 categories in 1991-2001." (Kirovgeologiya SE, Mr. Lysenko, Smolino city, 2002).
2. The report of the State Service of Geology and Mineral Resources of Ukraine as of April 31, 2002. #35 concerning registration by the Scientific Council for Forecasting on Stankuvatskyш and Nadiya prospectiveresources of Li2O class of 333 code by category P1 and 334 class code by category P2.

In addition, perspective resources by the categories of P1 and P2 of related components - Rb2O, Cs2O, Ta2O5, Nb2O5, BeO,SnO2 - have been accepted.

Resources/reserves assessment: In 2018, the State Commission on Mineral Reserves of Ukraine tested reserves and resources of lithium ores by categories C2, P1 and P2.

Separately, the State Commission on MineralReserves of Ukraine noted the presence in lithium ores of Dobra block prospective and projected resources of useful components - tantalum, niobium, rubidium, beryllium, tin and cesium. And information on thenumber of reserves and resources has limited access.

Here is the link:

https://www.geo.gov.ua/wp-content/uploads/2021/01/DOBRA_license.pdf

Taurisk