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- W2759475482 abstract "This chapter provides a reference for the increasing number of geologists who have little or no experience in the interpretation of natural and induced fractures in cores. Ideal, Andersonian intermediate-angle shear fractures and faults have 60° dip angles as well as slickenlines that record normal dip-slip offset. Intermediate-angle shears commonly occur in conjugate pairs with parallel strikes and opposing dip azimuths, although this may not be apparent unless lengths of core are removed from the core boxes and locked together end to end. Ideal intermediate-angle shears form where the weight of the overburden comprises the maximum compressive stress. Intermediate-angle compaction shears that form prior to lithification are common in muddy strata and can resemble the more planar, intermediate-angle shears formed under higher stress conditions after lithification. However, compaction shears, typically have undulatory surfaces and non-systematic strikes." @default.
- W2759475482 created "2017-10-06" @default.
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- W2759475482 date "2017-09-22" @default.
- W2759475482 modified "2023-10-14" @default.
- W2759475482 title "Intermediate-Angle Shear Fractures" @default.
- W2759475482 doi "https://doi.org/10.1002/9781119160014.ch8" @default.
- W2759475482 hasPublicationYear "2017" @default.
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