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Inventus Mining Corp V.IVS

Alternate Symbol(s):  GNGXF

Inventus Mining Corp. is a Canada-based exploration company. The Company is focused on the development of its gold and critical metals projects located east of the world class mining district of Sudbury, Ontario. The Company holds two 100% owned projects, Pardo Gold and Sudbury 2.0 Polymetallic Gold. The Pardo Paleoplacer Gold Project is located in Ontario, Canada, approximately 65 kilometers (km) northeast of the mining district of Sudbury. The Pardo Project consists of a 3.8 square kilometers (km2) block of mineral leases and 180 km2 of mineral claims covering the target paleoplacer geology. The Sudbury 2.0 Project is located east-northeast of Sudbury, Ontario. The property is accessible by road. The Sudbury 2.0 project consists of 240 km2 of mineral claims covering the Temagami Anomaly. The Company owns a 100% interest in the property. In addition, the Company, through Conquest Resources, holds claims to the east of the Sudbury 2.0 Project Area.


TSXV:IVS - Post by User

Comment by oceanelevenon May 10, 2021 2:25pm
131 Views
Post# 33166280

RE:RE:RE:RE:RE:Buy volume coming in ...

RE:RE:RE:RE:RE:Buy volume coming in ... Chief Geologist wesley is now VP of exploration!!! We are getting ready for 007!!!

The 2.45 to 2.2 Ga Huronian Basin in Ontario, Canada, has been thought to contain many similarities with the famous Witwatersrand goldfields in South Africa. Recent discoveries suggest the Huronian Basin may contain Witwatersrand-type gold deposits. The gold mineralization has been discovered within separate conglomeratic stratigraphy of both the Mississagi and Matinenda formations. These discoveries have developed into what is now known as the Pardo project in Pardo Township 65km northeast of the famous Sudbury mining camp. The basal Mississagi cobble to boulder conglomerates can contain values up to 542 g/t Au. The Pardo project is located in the eastern portion of the Huronian Basin known as the Southern Cobalt Embayment. The western portion of the basin, which is most analogous to the Witwatersrand, is historically known for its uraniferous quartz- pebble conglomerates of the Matinenda Formation at Elliot Lake.
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