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The relation between the crystallography of quartz, and upturned aeolian cleavage plates
Author(s) -
WELLENDORF WILLIAM,
KRINSLEY DAVID
Publication year - 1980
Publication title -
sedimentology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.494
H-Index - 108
eISSN - 1365-3091
pISSN - 0037-0746
DOI - 10.1111/j.1365-3091.1980.tb01193.x
Subject(s) - quartz , cleavage (geology) , geology , aeolian processes , sedimentary rock , mineralogy , abrasion (mechanical) , silt , scanning electron microscope , grain size , geomorphology , composite material , geotechnical engineering , materials science , geochemistry , paleontology , fracture (geology)
The relation between the crystallography of artificially abraded quartz sand grains and aeolian surface textures has been studied using an X‐ray precession camera and the scanning electron microscope (SEM). Crushed Brazilian quartz was sieved to between 250 and 350 μm, eroded in a paddle wheel device which simulated aeolian action at 8 m s −1 for 3 h, and photographed with the SEM. A typical grain was selected and over 1100 photographs were combined to create a 3 × 3 m photomosaic; because of the large size, it was possible to observe and measure the angular and linear relations between the various features. After the c axis direction in the grain was determined by precession X‐ray analysis, the most important aeolian features were related to the crystallography of quartz. The upturned plates or cleavage plates probably represent traces parallel to r (10Ī1) and z (01Ī1) cleavages in quartz. Blocky areas appear to be an expression of a cleavage parallel to m (10Ī0). In addition, plate spacing on thirty‐five experimental, modern, and ancient quartz sand grains is fairly constant. Assuming that abrasion in most sedimentary environments acts in the same manner with respect to quartz crystallography, much of the fine silt and clay in sediments and sedimentary rocks may be the result of cleavage following abrasion parallel to the r and z cleavage planes, while the less common blocky particles are probably the result of cleavage parallel to the m planes.