Petedunnite (CaZnSi2O6): Stability and phase relations in the system CaO-ZnO-SiO2

作者：Huber Alexandra L^*; Heuss As**ichler Soraya; Fehr Karl Thomas; Bromiley Geoffrey D

来源：American Mineralogist, 2012, 97(4): 739-749.

DOI：10.2138/am.2012.3836

• Zinc
• clinopyroxene
• petedunnite
• stability
• phase relations
• skarn
• petrogenetic indicator
• geobarometry
• experimental calibration

The phase relations of petedunnite [CaZnSi2O6 (pd)] were determined experimentally at P-T conditions up to 2.5 GPa and 1100 degrees C. Single-phase petedunnite is formed at high pressures (P %26gt; 0.8 GPa). Reversed experiments show that at lower pressures and temperatures %26gt;650 degrees C petedunnite decomposes to willemite [Zn2SiO4 (wil)], hardystonite [Ca2ZnSi2O7 (har)], and quartz [SiO2 (qtz)] according to the reaction 4 pd = wil + 2 har + 3 qtz. The boundary curve for this equilibrium reaction is given by P (GPa) = -0.093 (0.029) + 0.0014 (0.0003) T (degrees C), by disregarding the phase transition of quartz. The stability field of wil + bar + qtz is restricted toward lower temperatures by zinc-feldspar [CaZn-SiO8 (zfsp)] according to the known reaction: wil + 2 har + 7 qtz = 4 zfsp. These reactions intersect at 650(1) degrees C/0.78(0.01) GPa, generating an invariant point I-pd. Additionally, petedunnite-breakdown reaction is intersected by the low/high-quartz phase transition curve, generating an invariant point I-qtz(pd) at similar to 840 degrees C, 1.04 GPa. At temperatures %26lt;650 degrees C, further reactions occur in the system CaO-ZnO-SiO2 including the doubly degenerate reaction zfsp = pd + qtz and 3 pd = liar + wil + zfsp, which also intersect the invariant point I-pd. All reactions involving petedunnite display shallow positive slopes within the P/T-field, indicating that the crystallization of petedunnite is highly pressure sensitive over a wide temperature range. This means that an increasing petedunnite component in pyroxene shifts its stability field to higher pressures, similar to the effect of a jadeitic component. %26lt;br%26gt;The study of natural clinopyroxene and the correlation of its zinc content with published P-T conditions of these mineral assemblages confirmed a significant relationship between extraordinary high-zinc concentrations in pyroxene and high-metamorphic pressure conditions. In addition, the petedunnite component is obviously sensitive to the prevailing fluid conditions in terms of the fugacity ratio fs(2)/fo(2.) Furthermore, a distinct temperature dependency of the zinc component was observed in the range of trace element concentration. In consequence, Zn turns out to be a key element with regard to its implementation as a sophisticated petrogenetic indicator of metamorphic conditions. Therefore, routine measurement of zinc in element analyses of clinopyroxenes is strongly recommended.

• 出版日期2012-4