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Conclusions<br />
• Shap weathers by stoichiometric<br />
dissolution<br />
– Centred on reactive sites<br />
controlled by composition and/or<br />
strain<br />
– Leached layers must be < ~2 nm<br />
• Glen Feshie weathering products<br />
grow passively on grains from bulk<br />
waters<br />
– Some amorphous<br />
– Crystallises to form clays
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