Cross Lake Project (1983-86)
Geologist P.G. Lenton
Year 83
STATION 5001
EASTING 571846
NORTHING 6046645
ZONE 14
DATUM NAD83
Date of mapping 06/17/1983
STRUCTURAL DATA
| Layering type | Strike | Dip | top Direction |
|---|---|---|---|
| bedding | 286 | 71 | N |
| Structure type | Strike | Dip | Separation |
|---|---|---|---|
| schistosity | 286 | 71 |
| Rock Number | Type | Width (m) | Strike | Dip |
|---|---|---|---|---|
| 0 | pegmatite | 0.20 | 208 | 76 |
-slightly sheared quartz poor pegmatite
-photos bedding in gr. greywacke
-deformed, some boudinage 20 cm
PETROLOGIC DATA
Rock Number: 1
-Dominantly graded and parallel laminae layers with minor ripple layers.
-No E division numerous faserkiesel in semi pelite layers.
-Minor 10-30cm amphibolite layers
Turbidite
| Type | Mineral | Min. Size | Max. Size | Abundance (%) | Unit |
|---|---|---|---|---|---|
| faser kiesel | sillimanite | 1.0 | 10.0 | 4.0 | cm |
| groundmass grainsize | 0.0 | 0.5 | mm | ||
| bedding thickness | 1.0 | 10.0 | cm |
| Mineral | Abundance (%) |
|---|
| garnet |
| sillimanite |
Rock Number: 2
-As at 1st stop an amphibolitic wacke/tuff mixture.
-Mainly to south of greywacke
| Type | Mineral | Min. Size | Max. Size | Abundance (%) | Unit |
|---|---|---|---|---|---|
| mafic mineral | hornblende | 0.0 | 0.0 | 30.0 | |
| groundmass grainsize | 0.0 | 0.2 | mm |
| Mineral | Abundance (%) |
|---|
| hornblende |
| garnet |
Rock Number: 3
-Bright pink with a glassy look
-numerous dikes parallel to contact with granodiorite; range from 5 cm to 1 m in thickness
-scattered potassium feldspar megacrysts
| Type | Mineral | Min. Size | Max. Size | Abundance (%) | Unit |
|---|---|---|---|---|---|
| phenocryst | potassium feldspar | 0.0 | 0.0 | mm |
PHOTOS
Graded bedding in garnet-sillimanite bearing greywacke. Thin layer of hornblende-garnet+/-dioside amphibolite exhibits boudinage. Greywacke has disruption of layering and incipient mobilizate developing in the semi-pelitic beds.
As previous photo showing prefferential shearing an isoclinal folding in the bedding plane of the most pelitic beds.
Oblique view of previous photo
Manitoba Geological Survey, 2017