1 / 2

PROJECTS ASSESSMENT

PROJECTS ASSESSMENT. Kage Minerals and GL Jossue & JB Joel. SINGIDA-MAYAMAYA PROVINCE, LAKE VICTORIA GOLDFIELDS REGION. Target: Potential >500,000 oz Au deposits in tectonothermally-modified granitoid-greenstone domains and extensions to Shanta Gold’s 800,000 oz @ 2.84g/t Au deposit.

wanda
Download Presentation

PROJECTS ASSESSMENT

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. PROJECTS ASSESSMENT Kage Mineralsand GL Jossue & JB Joel

  2. SINGIDA-MAYAMAYA PROVINCE, LAKE VICTORIA GOLDFIELDS REGION Target: Potential >500,000 oz Au deposits in tectonothermally-modified granitoid-greenstone domains and extensions to Shanta Gold’s 800,000 oz @ 2.84g/t Au deposit Overview: Clients 1 (Kage Minerals: HQ-P 26609) in the Kwa-Mtoro Granitoid Domain and Client 2 (GL Jossue & JB Joel: PL 7838/12; PL5020/08; PL4934/08; HQ-P 22932) in the Sanzawa Greenstone Domain Geological Setting: The properties under review covers the north-western parts of the gold-hosting Kwa-Mtoro-Sanzawa Belt, whose bedrock geology is largely covered by Neogene volcanic and superficial deposits. Strongly deformed greenstones crop out, and those exposed by small-scale mining activities, comprise strongly mylonitic mafic amphibolite, meta-gabbro and meta-dolerite. Weakly deformed dark-green basaltic-andesite and porphyritic intermediate volcanic rocks are also partly covered by residual red soil and thin black cotton soils. Highlights: • Gold-endowment of the Singida-Mayamaya Province previously less-explored most probably due to: • strong late-Precambrian tectonothermal modification of the geology • Lodes of gold mineralisation previously mapped as fine-grained cataclasite (Fozzard (1959) • Exploration encouraged by ASM discoveries in the Kwa-Mtoro Granitoid Domain • Government’s support such as acquisition of high-resolution geophysical data including gravity and VTEM • Systematic exploration on London’s ASM discoveries led to SHANTA’s >800,000 Au (resource) discovery • Gold in the Sanzawa Domain occurs in quartz veins hosted by shear-foliated dolerite, mafic amphibolite • Gold in the Kwa-Mtoro Granitoid Domain occurs in strongly shear-foliated granitoid gneisses. • Both domains are bounded by NW-SE-trending crustal-scale structures and 2680 Ma granitoids. • A sinistral reactivation along these structures may have facilitated preferential development domain-scale structural traps. • Field visit to Kwa-Mtoro Sanzawa Properties undertaken in March 2014.

More Related