Abstract
Two different types of interstratified illite-smectite are found in a section of Paleozoic sediments in the Negev, Israel. One of these is detectable only by a decrease in peak width and a concomitant increase in symmetry of the 10 Å peak on glycolation. This material is regarded as illite, randomly interstratified with about 20 per cent expanding layers.
Original language | English |
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Pages (from-to) | 165-168 |
Number of pages | 4 |
Journal | Clays and Clay Minerals |
Volume | 20 |
Issue number | 3 |
DOIs | |
State | Published - Jun 1972 |