| 1. | Clay minerals have a significant effect on the adsorption of energetic compounds.
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| 2. | In effect, the clay minerals replicated the structure of the living tissues.
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| 3. | Clay minerals continue to be formed as long as the soil exists.
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| 4. | It can occur intermixed with dickite, kaolinite, montmorillonite and other clay minerals.
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| 5. | The common clay minerals are montmorillonite or smectite, illite, and kaolinite or kaolin.
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| 6. | Here, orbiting instruments have detected signatures of both clay minerals and sulfate salts.
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| 7. | Feldspar, amphiboles, pyroxenes, and volcanic glass are the principle donors of clay minerals.
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| 8. | X-ray diffraction pattern of a Nontronite standard purchased from the clay mineral society.
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| 9. | It also includes an area where clay minerals have been detected from orbiter observations.
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| 10. | During a deluge, slopes grow heavy and water lubricates clay minerals in the soil.
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