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Fe-Zn-S system and the sphalerite geobarometer

Fe-Zn-S system and the sphalerite geobarometer

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How do we get <strong>the</strong>m out?<br />

� Carbonates: phosphoric acid -> CO 2<br />

� Silicates: reaction w/ BrF 5, F 2, ClF 3 -> O<br />

� O + hot graphite -> CO 2<br />

� Sulfides: heat w/ oxidant e.g. CuO<br />

� S + O -> SO 2<br />

� Or S + F source -> SF 6<br />

� OH or H 2O: reaction w/ hot U or <strong>Zn</strong> -> H 2<br />

� Now: Direct laser fluorination<br />

Ratios: Del/Delta Terminology<br />

� δO 18 , δD, δC 13 , δS 34<br />

� δ = (R sample/R std -1) * 1000<br />

� where<br />

� R sample = (O 18 sample /O16 sample )<br />

� Ex: a δ of +10 => sample 1% heavier than<br />

<strong>the</strong> st<strong>and</strong>ard<br />

St<strong>and</strong>ards<br />

� Very difficult to measure absolute<br />

amounts so always use st<strong>and</strong>ards<br />

allowing ratio measurements<br />

� O & H: referred to SMOW<br />

� Soft rockers may refer O to PDB<br />

� C: belemnite from <strong>the</strong> Pee Dee Fm: PDB<br />

� S: Canyon Diablo meteorite troilite: CDT<br />

Fractionation Factors<br />

� See reading for relationship of <strong>the</strong> delta<br />

notation to more rigorous derivation of <strong>the</strong><br />

fractionation factor between 2 minerals or<br />

phases yielding diagrams with axis of:<br />

� 10 3 lnα A-B<br />

� 10 3 lnα A-B ~ δ A - δ B = Δ AB<br />

2

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