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- W1997169029 abstract "The upper three-fourths of the White Pine Group (Late Mississippian) at four widely separated and representative sections in eastern Nevada is characterized by illitic mixed-layer clay, whereas the lower fourth is characterized by well-crystallized illite and, at two of the four sections, by dolomite. These distinctive mineral assemblages meet at a sharply defined, easily determinable boundary that can serve as a stratigraphic marker within this thick, in places poorly exposed, commonly lithologically similar sequence. This boundary can be extended westward to a fifth section if one accepts that the clay minerals in the fifth locality have been affected by incipient metamorphism." @default.
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- W1997169029 date "1969-01-01" @default.
- W1997169029 modified "2023-09-27" @default.
- W1997169029 title "Mineralogic Stratigraphic Marker in White Pine Group, Eastern Nevada: GEOLOGICAL NOTES" @default.
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- W1997169029 doi "https://doi.org/10.1306/5d25c6a9-16c1-11d7-8645000102c1865d" @default.
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