An Experimental Investigation Into the Flow of Marble
An Experimental Investigation Into the Flow of Marble
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The proportion of grains which show it is no greater in the deformed than in the original limestone. What cleavage is visible was probably developed during the grinding of the section, as it is seen in 3 c 2 380 PROFESSOR F. D. ADAMS AND DR. J. T. NTCOLSON places in sections of all marbles. There has been no breaking the rock has not been crushed in the ordinary sense of the term. The movement has been brought about partly by twinning but chiefly by a deformation of the grains due to a slipping... on their gliding planes. The structure is essentially that presented by those portions of the marble lying between the lines of granulated calcite in the case of the marble deformed at the ordinary temperature. In the accompanying plates, mierophoto- graphs of the marble before and after deformation at 300 C. Are shown.
Plate 24, fig. 1, shows the appearance of a thin section of the original Carrara marble in ordinary light, magnified 50 diameters. The individuals are approximately equidimensional, and only three or four show twinning.
What to read after An Experimental Investigation Into the Flow of Marble?
You can find similar books in the "Read Also" column, or choose other free books by Frank Dawson Adams to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
The proportion of grains which show it is no greater in the deformed than in the original limestone. What cleavage is visible was probably developed during the grinding of the section, as it is seen in 3 c 2 380 PROFESSOR F. D. ADAMS AND DR. J. T. NTCOLSON places in sections of all marbles. There has been no breaking the rock has not been crushed in the ordinary sense of the term. The movement has been brought about partly by twinning but chiefly by a deformation of the grains due to a slipping... on their gliding planes. The structure is essentially that presented by those portions of the marble lying between the lines of granulated calcite in the case of the marble deformed at the ordinary temperature. In the accompanying plates, mierophoto- graphs of the marble before and after deformation at 300 C. Are shown.
Plate 24, fig. 1, shows the appearance of a thin section of the original Carrara marble in ordinary light, magnified 50 diameters. The individuals are approximately equidimensional, and only three or four show twinning.
What to read after An Experimental Investigation Into the Flow of Marble?
You can find similar books in the "Read Also" column, or choose other free books by Frank Dawson Adams to read onlineMoreLess
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