Zobrazeno 1 - 10
of 40
pro vyhledávání: '"Albert Johannsen"'
Autor:
Albert Johannsen, C. A. Merritt
Publikováno v:
The Journal of Geology. 34:275-280
Various rock minerals were crushed and sifted to determine the relative losses through different sieves. It was found that these losses were not equal in different minerals, so that discarding the fines may introduce errors in proportions in percenta
Publikováno v:
The Journal of Geology. 22:625-629
Autor:
Albert Johannsen
Publikováno v:
The Journal of Geology. 36:283-286
North American igneous rocks are shown to be universally lighter in color (and therefore also in density) than European rocks of the same kind. Curves are given showing this color difference for granites, granodioritic-granites, rhyolites, gabbros, a
Autor:
Albert Johannsen, Albert D. Brokaw
Publikováno v:
The Journal of Geology. 20:80-90
Autor:
T. C. Phemister, Albert Johannsen
Publikováno v:
The Journal of Geology. 33:268-271
The Gaston rebound tester is used to determine the relative elasticities of various minerals. Under this test fluorite, pyrite, quartz, and garnet are shown to be more elastic than steel. The remarkable rebound of 97 per cent was obtained on garnet,
Autor:
Albert Johannsen
Publikováno v:
The Journal of Geology. 27:276-285
Autor:
Albert Johannsen
Publikováno v:
The Journal of Geology. 19:317-322
It is obvious that a considerable part of the system of classification and nomenclature here proposed can only be applied upon microscopical or chemical investigation. .... For these reasons . . . . we are convinced of the need of general petrographi
Autor:
Albert Johannsen, L. H. Adams, E. D. Williamson, E. T. Allen, E. G. Zies, B. Asklund, J. Austen Bancroft, W. V. Howard
Publikováno v:
The Journal of Geology. 34:475-478
Autor:
Albert Johannsen
Publikováno v:
The Journal of Geology. 35:270-275
The terms "diabase" and "dolerite" are used with various meanings in different countries. In this paper the development of the terms is traced.
Autor:
Albert Johannsen, T. C. Phemister
Publikováno v:
The Journal of Geology. 32:81-84
A method is presented which to a large extent eliminates the errors of observation of the optic axial angle by the Michel-Levy method. Instead of standardizing circles of reference, observations on a mineral of known 2E are made directly through the