The Banket a Study of the Auriferous Conglomerates of the Witwatersrand And the
The Banket a Study of the Auriferous Conglomerates of the Witwatersrand And the
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3). A slight degree of shifting among the segments causes distortion of the pebbles. The fracturing of the associated quartzites appears to be in general less complicated and more widely spaced than in the banket. This is probably due to the greater homogeneity of the former rock.
Distortion of pebbles of a different character to that just referred to is sometimes seen, especially in proximity to faults. The pebbles may be markedly drawn out, as is common in intensely sheared con- glomerates, a...nd, if close to a fault, bent in the direction of the movement that has taken place (Plate IX. , Figs, i and 2). Careful attention to this bending, even where it is very slight, is often sufficient to solve some of the difficult faulting problems that are encountered in the course of mining. Microscopic examination of a vein-quartz pebble thus drawn out and bent showed it to consist of a moderately fine- grained mosaic, in which the quartz grains were full of minute inclusions, except in narrow zones round their margins, which were clear.
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To quickly assess the difficulty of the text, read a short excerpt:
3). A slight degree of shifting among the segments causes distortion of the pebbles. The fracturing of the associated quartzites appears to be in general less complicated and more widely spaced than in the banket. This is probably due to the greater homogeneity of the former rock.
Distortion of pebbles of a different character to that just referred to is sometimes seen, especially in proximity to faults. The pebbles may be markedly drawn out, as is common in intensely sheared con- glomerates, a...nd, if close to a fault, bent in the direction of the movement that has taken place (Plate IX. , Figs, i and 2). Careful attention to this bending, even where it is very slight, is often sufficient to solve some of the difficult faulting problems that are encountered in the course of mining. Microscopic examination of a vein-quartz pebble thus drawn out and bent showed it to consist of a moderately fine- grained mosaic, in which the quartz grains were full of minute inclusions, except in narrow zones round their margins, which were clear.
What to read after The Banket a Study of the Auriferous Conglomerates of the Witwatersrand And the?
You can find similar books in the "Read Also" column, or choose other free books by Robert Burns Young to read onlineMoreLess
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