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        "sample_type":"outcrop specimen",
        "sampling_method":"outcrop sampling",
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        "stratigraphic_unit":"Cymbric Vale Formation",
        "geological_province":"Delamerian Orogen",
        "sample_remark":"near the middle of a bedded tuffaceous sequence. There are several limestone olistoliths up to 20 m across that have been reported to contain the Early Cambrian (Botomian-Atdabanian) archaeocyathids in the general vicinity. The rocks in this vicinity are all light coloured pyroclastic felsic tuffs that show indications of redeposition. At the collection site two parallel beds about 1 m thick show sharp basal contacts and graded finer grained tops. Most of the beds are of coarse sand size with scattered larger pyroclastic fragments up to 3 cm. The rocks are solid and non-porous and of low metamorphic grade. Most beds show pale green fragments that are probably coloured by the mineral celadonite. Bedding at the collection site dips at 50 degrees to 334 true and faces northwest on the grading. These observations are characteristic of a wide area here and the absence of rock cleavage suggests that the regional folds are fairly broad and open in shape. The rock appears to be totally non-magnetic.",
        "earth_materials":"Y",
        "structural_measurements":null,
        "inorganic_geochemistry":null,
        "organic_geochemistry":null,
        "geochronology":"Y",
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        "rock_properties":null,
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        "sample_originator":"Jagodzinski, E.A.",
        "date_acquired":null
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