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- W2190949228 abstract "DEFORMATION PROCESSES IN SANDSTONE AND OTHER ROCKS WERE STUDIED MICROSCOPICALLY AND WITH AN OSCILLOSCOPE. THE SPECIMENS WERE DEFORMED UNDER SEVERAL STAGES OF CONFINING PRESSURE: 500 BARS (BRITTLE), 1000 BARS (TRANSITIONAL), 1500 BARS (DUCTILE). FISSURES APPEARED AT THE EARLY STAGES AND WERE PROPORTIONAL TO THE RESIDUAL STRAIN. MICRO-FISSURE ANGLES VARIED FROM 0 TO 45 DEGREES AND WITH INCREASING PRESSURE BECAME CONCENTRATED IN NARROW BANDS AT AN ANGLE OF 30-40 DEGREES WITH THE AXIS OF MAXIMUM COMPRESSION. AS THE STRESS-STRAIN CURVE RISES TO THE MAXIMUM POINT, MACRO-FRACTURES DEVELOP PARALLEL TO THESE DEFORMATION BANDS." @default.
- W2190949228 created "2016-06-24" @default.
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- W2190949228 date "1970-01-01" @default.
- W2190949228 modified "2023-09-27" @default.
- W2190949228 title "PROCESS OF DEFORMATION OF THE SEDIMENTARY ROCKS" @default.
- W2190949228 hasPublicationYear "1970" @default.
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