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- W2034874592 abstract "Oriented granite cores from the Illinois borehole UPH-3 contain planes of secondary fluid inclusions, which represent healed microcracks. They record the orientation of a paleostress field, with the maximum stress in the horizontal plane oriented to the NNW about 90° from the present stress field orientation. These bubble planes probably formed while the granite was still quite warm (> 400° C) during initial cooling, uplift, and unroofing of the granite prior to deposition of younger overlying Cambrian sediments. The bubble planes have a much more uniform orientation than the open microcracks, which formed by stress-relief when the core was removed from the borehole." @default.
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- W2034874592 date "1987-04-01" @default.
- W2034874592 modified "2023-10-16" @default.
- W2034874592 title "Healed microcrack orientations in granite from Illinois borehole UPH-3 and their relationship to the rock's stress history" @default.
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- W2034874592 doi "https://doi.org/10.1016/0040-1951(87)90114-4" @default.
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