Allendeite (Sc4Zr3O12) and hexamolybdenum (Mo,Ru,Fe), two new minerals from an ultrarefractory inclusion from the Allende meteorite

作者：Ma Chi^*; Beckett John R; Rossman George R

来源：American Mineralogist, 2014, 99(4): 654-666.

DOI：10.2138/am.2014.4667

• Allendeite
• Sc4Zr3O12
• hexamolybdenum
• new alloy
• new mineral
• EBSD
• nanomineralogy
• Allende meteorite
• CV3 carbonaceous chondrite

During a nanomineralogy investigation of the Allende meteorite with analytical scanning electron microscopy, two new minerals were discovered; both occur as micro- to nano-crystals in an ultrarefractory inclusion, ACM-1. They are allendeite, Sc4Zr3O12, a new Sc- and Zr-rich oxide; and hexamolybdenum (Mo,Ru,Fe,lr,0s), a Mo-dominant alloy. Allendeite is trigonal, R (3) over bar, a = 9.396, c = 8.720, V = 666.7 angstrom(3), and Z = 3, with a calculated density of 4.84 g/cm(3) via the previously described structure and our observed chemistry. Hexamolybdenum is hexagonal, P6(3)/mmc, a = 2.7506, c = 4.4318 angstrom, V = 29.04 angstrom(3), and Z = 2, with a calculated density of 11.90 g/cm(3) via the known structure and our observed chemistry. Allendeite is named after the Allende meteorite. The name hexamolybdenum refers to the symmetry (primitive hexagonal) and composition (Mo-rich). The two minerals reflect conditions during early stages of the formation of the Solar System. Allendeite may have been an important ultrarefractory carrier phase linking Zr-,Sc-oxides to the more common Sc-,Zr-enriched pyroxenes in Ca-Al-rich inclusions. Hexamolybdenum is part of a continuum of high-temperature alloys in meteorites supplying a link between Os- and/or Ru-rich and Fe-rich meteoritic alloys. It may be a derivative of the former and a precursor of the latter.

• 出版日期2014-4