By Neal R. O’Brien, Roger M. Slatt (auth.)
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An interesting observation in our study of lamination in black shales is that lamina thickness is not regular but varies vertically throughout a unit. JET ROCK SHALE FORMATION (Upper Lias, Jurassic) Raven scar, Yorkshire, England. This section presents a detailed analysis of the composition and fabric of a typical lamina couplet of alternating fine-coarse material in the black Jet Rock Shale. The purpose is to show the usefulness of microanalysis in obtaining evidence of the origin of black shale and, in particular the origin of lamination.
SUNBURY FORMATION (Mississippian) Gallia County, Ohio. This shale exhibits well developed parallelism of platy material. Scale = 10 /lm. SCANNING ELECTRON MICROSCOPY DESCRIPTIONS·PREFERRED PARTICLE ORIENTATION IN SHALE c A B D 25 RANDOM PARTICLE ORIENTATION IN MUDSTONE A. FLOCCULATED ILLITE - This stereo micrograph shows the fabric of grundite illite (1 gm/l ) flocculated in salt water (27 NaCl gm/l), sedimented in a glass tube, and air-dried. Randomness of domains plus some individual flakes prevails in this sample.
1986). ). The finely- to thickly-laminated character of the Jet Rock Shale suggests another mechanism. During the deposition of the Jet Rock shale, conditions were such that continuous sedimentation of organic-rich clay was periodically interrupted by deposition of silt. Lamination in this example provides evidence of systematic alternation of sedimentary conditions, possibly indicating periodic pulses of coarser sediment deposited rapidly into the anaerobic environment. %. 8 44 C 1. SEM photograph of microfabric of a typical silt-rich layer.
Argillaceous Rock Atlas by Neal R. O’Brien, Roger M. Slatt (auth.)