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" The country rock is jasper, thin layered and separated by seams of shale. The jasper layers differ in thickness from a fraction of an inch to several feet. The same layer varies in thickness, pinching out locally In many places. Most of the shale seams... "
Bulletin of the United States Geological Survey - Seite 161
von Geological Survey (U.S.) - 1910
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Muscovite in the Spruce Pine District, North Carolina, Ausgabe 936

Thomas Lingle Kesler, Jerry Chipman Olson - 1942 - 496 Seiten
...schist is generally not distinct; the two are commonly separated by a transitional zone which varies in thickness from a fraction of an inch to several feet. The topaz rock retains either a faint banding (see pi. 8, B) or the pattern of a breccia (see pi. 8, (3),...
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Nuclear Science Abstracts

1960 - 1118 Seiten
...area the veins — called "siliceous reefs" — strike east to northeast, are of steep dip, and vary in thickness from a fraction of an inch to several feet. The country rock is granodiorite containing, in order of abundance, plagioclase (Anw to AnM), quartz, orinecíase,...
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Bulletin, Ausgabe 670

1918 - 72 Seiten
...dirtygray sandstone containing thin calcareous beds and numerous lenses and layers of sandy shale ranging in thickness from a fraction of an inch to several feet. The distribution of the oil in the sand is probably dependent to a considerable degree on differences in...
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Report No. FHWA-RD.

United States. Federal Highway Administration. Offices of Research and Development - 1976 - 552 Seiten
...foot (ll.5 m) beds of conglomerate and sandstone with interbeds of shale and siltstone which range in thickness from a fraction of an inch to several feet. The thick-bedded conglomerate and sandstone are well cemented by quartz, chalcedony, and iron oxide, and...
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