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- W2001044487 abstract "A building founded on Billings Shale has suffered nearly 4 in. (10 cm) of heave to its basement floor slab. The heaved zone was thought to be associated with a fault zone in the shale, ear which the rock was fractured and contained extensive pyrite intrusions. Investigations have shown the heave to be due to the weathering of the pyrite in the presence of autotrophic bacteria. Factors creating a favorable environment for this complex weathering process are discussed." @default.
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- W2001044487 date "1970-08-01" @default.
- W2001044487 modified "2023-09-26" @default.
- W2001044487 title "Investigation of heave in Billings shale by mineralogical and iogeochemical methods" @default.
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- W2001044487 doi "https://doi.org/10.1139/t70-040" @default.
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