By A.E. Adams
Offers a truly transparent advisor to sedimentary rock kinds as visible less than the microscope supported via useful points of slide practise.
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Extra info for Atlas of Sedimentary Rocks Under the Microscope
Such a cement. being aragonite. is not likely to be well-preserved in an ancient limestone. If it undergoes neomorphism (p. 60), the overall radial-fibrous fabric may be retained although detatl will be lost. In the sample shown, there is a second generation of pink-stained fine sparite infilling pores. This is typical of cement deposited from meteoric waters. 127 shows a limestone in which there arc also two cement generations. The first appears as a rim of crystals of equal thickness on all grains (about 2 mm in width in the photograph).
29 Terrigenous clastic rocks 68,69 Si ltstones Siltstones are those terrigenous sediments in which the majority of the grains are between 16 and 2� 6 mm in diameter (Table I , see p. 3). 68 and 69 show a coarse siltstone (notice that the magnification is higher than that of most of the previous photographs) with abundant quart£ grains and thin mica flakes. The micas include both muscovite (colourless) and biotite (yellow or brown). Muscovite is more abundant and shows second order interference colours.
54 and 55 �how a �cdimcnt in which more than 50% of the grams arc feldspar. easily Identifiable in PPL by the broY. n colour rcsuhmg from their alteration (see p. 7) and in cros�cd polars by the remnants of multiple \\\inning in many grains. Most of the other grains in the sediment arc clear quart;. so the sample is an arkose. A sediment with such a high proportion of relatively unstable feldspar grains is mineralogically immature. The matrix coni