Mineral Deposit Inventory for Ontario

Ministry of Energy, Northern Development and Mines

Permanent Link to this Record: MDI000000002304

Deposit: MDI000000002304

General

Mineral Deposit Identification
Deposit Name(s) Ferraro - 2009
Deposit Status occurrence
Date Created 2019-Jul-26
Date Last Modified 2019-Jul-26
Created By T Pettigrew
Revised By T Pettigrew

Commodities

Primary Commodities: gold, copper

Location

Township or Area: Ashmore

Latitude: 49° 40' 36.81"    Longitude: -86° 50' 11.99"

UTM Zone: 16    Easting: 511784   Northing: 5502720    UTM Datum: NAD83

Resident Geologist District: Thunder Bay North

NTS Grid: 42E10NW

Point Location Description: From trench samples in Assessment report 20000006338

Location Method: data compilation

Exploration and Mining History

2009: S. Shields carried out prospecting and sampling and discovered the zone. 2009-10: Prodigy Gold carried out prospecting and sampling.

Assessment Work on File

Assessment Work on File
Office File Number   Online Assessment File Identifier   Online Assessment File Directory  
2.47854     20000006767     Open
2.47964     20000006338     Open

Geology

Province: Superior

Subprovince: Wabigoon

Belt: Beardmore-geraldton

Geological Age: Archean   

Mineral Deposit Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
mafic metavolcanics 1 near
vein 2 quartz host
mafic intrusive 3 gabbro near

Lithology Comments

07/26/2019 (T Pettigrew) - There are two small weak to moderate shear zones within the Ferraro Zone. Both of the shear zones are only present within the mafic metavolcanics and seem to dissipate within the gabbros. The northern shear zone has a strike of 102 degrees and a dip of 85 degrees dipping south. Towards the western edge of the trench the shear direction shifts to an 080 degree strike, and vertical dip. The southern shear zone has a strike of 098 degrees, and a dip of 75 degrees dipping south, and seems to be an extension of the quartz vein which sampled at 292 g/t Au. There are also three distinct fracture directions, mostly visible within the mafic metavolcanics, but also present in the gabbros. The three fracture directions are 001 degrees dipping 80 degrees to the east, 080 degrees dipping 82 to the south and 340 degrees dipping 77degrees to the east, the second of which seems to parallel some of the shear, and quartz veining.

Mineralization

Deposit Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Habit Description
1 gold economic ore
2 pyrite economic ore
3 pyrrhotite economic ore
4 chalcopyrite economic ore
1 quartz economic gangue
2 tourmaline economic gangue

Mineralization Comments

07/26/2019 (T Pettigrew) - The Ferraro Zone trenched area is 35 m long. The zone strikes east-west and is characterized by a thin mineralized quartz vein. The gold mineralization is confined to smoky grey, sulphidized, weakly fractured quartz veins, and the immediate sulphidized wallrock. The quartz vein with strong gold mineralization is approximately 20 m in length, and less than 15 cm in width. The quartz vein crosses the mafic metavolcanic unit, and the gabbro unit. The sulphides mineralization consists of disseminated pyrite, pyrrhotite, and chalcopyrite both within the quartz vein, and the surrounding wallrock. There are several specs of visible gold in the vein, mostly localized to a section of the vein 25 cm long A sample from the quartz-tourmaline vein assayed 292 g/t Au with 35.4 g/t Ag and 3.24% Cu. Channel sample highlights include 37.18 g/t Au over 0.80 m including 196 g/t Au over 0.15 m (Assessment file 20000006338).

Report an Error

We are continuously updating the Mineral Deposit Inventory. If you notice errors in the data please contact us.

Terms of Use

Please review our Terms of Use agreement for this data product.

Ministry Contact Information

For detailed information regarding this mineral deposit please contact the Thunder Bay North Resident Geologist District Office