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. 2012 Apr 4;3:134. doi: 10.3389/fmicb.2012.00134

Figure 4.

Figure 4

Mineralogy of Shovelers Sink clay size fraction. (A) TEM image showing flakes of smectite-dominated clay minerals (I/S), quartz (Qz), potassium feldspar (KF), plagioclase, and titania (TiO2) grains. (B,C) HRTEM image and selected area diffraction pattern taken from the area indicated by the large arrow in (A), showing the curled edge of a clay aggregate with lattice fringes corresponding to (001) smectite with ca. 10-Å layer spacing; the size of this spacing was likely reduced in the vacuum of the TEM. (D) EDAX results for an I/S aggregate. A small amount of potassium is detected, indicating that the smectite contains an illite component.