GEOMAGNETIC
EXPLORATION SURVEY
REPORT
Munyash Ventures Pvt Ltd
Goldcot Mining Consultancy
Ii 2018
Introduction
Munyash Ventures Pvt Ltd are acquired claims over the Chakari, Kadoma area in Mashonaland
West with the view to explore and mine for potential gold mineralized ore bodies. The claim
holders also envisaged the possibility of finding gold reserves that can be mined by open pit or
underground mining methods.
There are other small scale miners around Chakari, Kadoma area in Mashonaland West
purportedly owning gold claims and Juno 40 mine is in the capacity of identifying the viably
minable reefs within the claim.
Basic details of the mine in question are as indicated below:
Name of mine: Juno 40 mine
Registration No,
Area: Chakari, Kadoma
Mining background
This report is based upon the findings, observations and recommendations of a mine technical
survey that was conducted on the 11th of July 2018. The mine was operating with a greater risk
of failure to recover invested capital since the ore reserves were not well established and
therefore no structure of the plan set to determine how to explore the ore.
Areas of interest on the conducted technical survey:
Mine geology, i.e. Possibility of gold reef existence, possible locations, possible grade and
possible direction and depth of the gold reefs
Recommended site of shaft : They is a shaft which is about 6m
The mining method recommended against lowest possible costs and maximized safety
Regional Geology
The geology of Zimbabwe in Southern Africa is centered on the Zimbabwe Craton, a core of
Archean basement composed in the main of granitoids, schist and gneisses. It also incorporates
greenstone and bluestone belts comprising mafic, ultramafic and felsic volcanic which are
associated with epiclastic sediments and
Iron formations. The craton is overlain in the north, northwest and east by Proterozoic and
Phanerozoic sedimentary basins whilst to the northwest are the rocks of the Magondi
Supergroup. Northwards is the Zambezi Mobile Belt and to the east the Mozambican Belt.
South of the Zimbabwe Craton is the Kaapval Craton separated from it by the Limpopo Mobile
Belt, a zone of deformation and metamorphism reflecting geological events from Archean to
Mesoproterozoic times. The Zimbabwe Craton is intruded by an elongate ultramafic/mafic
igneous complex known as the Great Dyke which runs for more than 500km along a SSW/NNE
oriented graben. It consists of peridotites, pyroxenites, norites
and bands of chromitite. Gold mineralization is mostly associated with the granite greenstone
belts though rarely it has been mined in other geologic settings but the Karoo.
1. DOCUMENTARY MANDATE
This Report is strictly surrendered to the owner of the mine soon after preparation and
disclosure of the document to anyone who is not registered as the claim holder means the
breach of contractual obligations.
All the content of this document are technical observations and recommendations poised by a
trained personnel in that field with the assistance of instruments designed to bring a traceable
mineral exploration.
The mine owner is obliged to follow suit the instructions and safety standards posed by the
mining technician with licensed personnel in areas were blasting is required.
2. TERMS OF ENGAGEMENT
Munyash Ventures Pvt Ltd asked for a preliminary geological mineral reserves/ resources
evaluation of industrial sands deposit in the area currently within their mining boundaries using
currently available data. A site visit was conducted by the geologists to assess the deposit.
Goldcot Mining Consultancy Company has no direct nor indirect interests in the mine company.
3. OWNERSHIP
Juno 40 mine is wholly owned by Munyash Ventures Pvt Ltd a registered small scale miner with
the Ministry Of Mines And Mining Development in Zimbabwe.
REPORT COMPILED BY
Hadjieh Serez
(Mining Technician)
(0771716186/ 0785806177)
