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Publikováno v:
Geofluids, Vol 2021 (2021)
The presence of lamination on sedimentary rocks is a distinct characteristic, particularly in shales. They are distinct due to the contrast between successive layers with regard to grain size, composition, color, and sedimentary structures, such as g
Autor:
Stephen R. Hicock, C A Ozyer
Publikováno v:
Geochemistry: Exploration, Environment, Analysis. 11:335-350
Identification of kimberlite indicator mineral dispersal trains in glaciated terrain provides important clues in determining provenance. Complex ice flow history can distribute kimberlite indicator minerals such that dispersal trains are disguised wi