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Event details
Voyage: | IN2020_V01 [details] |
When: | 2020-02-03 15:20:35 UTC |
Log: | Geology_Rocks_in2020_v01 |
Equipment: | Not specified |
Position: | Latitude: -53.5213 Longitude: 83.0404 Position from underway logging |
Sample number: | IN2020_V01_D06_003 |
Dredge: | D06 |
Sample Number Assigned: | Yes |
Sample photographed (include scale and sample number): | Yes IN2020_V01_D06_003 |
Number of photos: | 3 |
Sample sawn: | Yes |
Sticker: | yes |
Colour: | brown | yellow |
Composition: | other |
Alteration: | Mn crust | altered |
Phenocryst mineralogy: | other |
Phenocryst abundance (%): | 0 |
Mn crust thickness (mm): | 12 mm |
Vesicle abundance: | absent |
Grain size: | pebble (2-64 mm) |
Grain shape: | angular |
Sorting: | moderate |
Components: | volcanic non-vesicular | continental lithic |
Sample bagged: | yes |
Bucket number: | D05/D06 1 of 1 |
Rock name: | Clay altered breccia |
Original Sample Dimensions: | 10 x 9 x 10 cm |
Comments: | Breccia clasts may be lithic fragments, or basalt; intense alteration prevents identification. Or this may be a pseudo-breccia. Looks like lithic fragment breccia, or pseudo breccia, which has been intensly clay altered. The breccia clasts look angular and moderately well-sorted |