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- W2018189980 abstract "Geostatistical image analysis of backscattered electron microscope (BSEM) images has been used to determine the degree of alignment (anisotropy) of clay minerals in late Tertiary mudstone samples from a range of depths from the Gulf of Mexico. This has been tied to mineral chemical analysis using secondary X-rays to determine whether fabric development is related to mineral diagenesis. Although compacted, mudstones at ∼ 5100 m have isotropic clay fabrics. Thousands of meters of overburden and the resulting stress have not induced the development of aligned fabric in mudstones. Mudstones adopt a progressively more anisotropic fabric with increasing depth of burial to ∼ 5600 m. Smectite is progressively replaced by illite with increasing depth over the same interval so there is a close correspondence between the illitization of smectite and fabric development. The fabric seems to be a consequence of mineral diagenesis. The kinetically controlled illitization of smectite has facilitated the development of fabric which is thus likely to be due to a dissolution and reprecipitation process rather than a solid-state process. Fabric development, with its consequences for porosity and permeability, is thus more likely to be a function of temperature and the thermal history rather than just depth and effective stress." @default.
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- W2018189980 date "2003-05-01" @default.
- W2018189980 modified "2023-09-26" @default.
- W2018189980 title "Fabric development and the smectite to illite transition in Gulf ofMexico mudstones: an image analysis approach" @default.
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- W2018189980 doi "https://doi.org/10.1016/s0375-6742(03)00073-6" @default.
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