Abstract
Nuwaite (Ni6GeS2, IMA 2013-018) and butianite (Ni6SnS2, IMA 2016-028) are two new chalcogenide minerals, occurring as micrometer-sized crystals with grossular, Na-bearing melilite, heazlewoodite, and Ge-bearing Ni-Fe alloys in veins and as mono-mineralic crack-filling material in igneous diopside in the Type B1 Ca-Al-rich inclusion (CAI) ACM-2 from the Allende CV3 carbonaceous chondrite. The chemical composition of type nuwaite is (wt%) Ni 65.3, S 10.3, Ge 8.2, Te 7.9, Sn 5.1, and Fe 1.7, with a sum of 98.5 and an empirical formula of (Ni5.95Fe0.16)(Ge0.60Sn0.23)(S1.72Te0.33). The simplified formula is Ni6(Ge,Sn)(S,Te)2, leading to an end-member of Ni6GeS2. The chemical composition of type butianite is (wt%) Ni 62.1, Sn 8.9, Te 10.3, S 8.9, Ge 5.3, Fe 1.3, sum 99.1, giving rise to an empirical formula of (Ni5.93Fe0.13)(Sn0.52Ge0.41)(S1.56Te0.45). Butianite’s simplified formula is Ni6(Sn,Ge) (S,Te)2 and the end-member formula is Ni6SnS2. Both nuwaite and butianite have an I4/mmm inter-growth structure with a = 3.65 Å, c = 18.14 Å, V = 241.7 Å3, and Z = 2. Their calculated densities are 7.24 and 7.62 g/cm3, respectively. Nuwaite and butianite are the first known meteoritic minerals with high Ge and Sn concentrations.
Nuwaite and butianite are very late-stage, vapor-deposited, alteration products, filling in pores within preexisting grossular-rich alteration veins and cracks in igneous Al,Ti-diopside. These phases and associated heazlewoodite and Ge-bearing alloys are observed only within the Ca-,Al-rich inclusion (CAI) and not outside it or at the inclusion-matrix interface. As only sections in one half of ACM-2 contain nuwaite/butianite, they were probably derived through a relatively low fO2-fS2 sulfidation process, in which a highly localized, low-temperature Ge-, Sn-bearing fluid interacted with a portion of the host CAI. It is likely that the fluid became relatively more Sn- and Te-enriched with time and that crack fillings post-date vein fillings, possibly due to a late remobilization of vein sulfides.
Acknowledgments
SEM, EBSD, and EPMA analyses were carried out at the Caltech GPS Division Analytical Facility, which is supported, in part, by NSF Grants EAR-0318518 and DMR-0080065. J.R.B. acknowledges NASA grant NNG04GG14G. We thank Klaus Keil, Mike Zolensky, and associate editor Steven Simon for helpful reviews.
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Articles in the same Issue
- Letter
- Rapid solid-state sintering in volcanic systems
- How geometry and anisotropy affect residual strain in host-inclusion systems: Coupling experimental and numerical approaches
- Special collection: Earth analogs for martian geological materials and processes
- Diverse mineral assemblages of acidic alteration in the Rio Tinto area (southwest Spain): Implications for Mars
- Special collection: From magmas to ore deposits
- Archaean hydrothermal fluid modified zircons at Sunrise Dam and Kanowna Belle gold deposits, Western Australia: Implications for post-magmatic fluid activity and ore genesis
- Special collection: Water in nominally hydrous and anhydrous minerals
- New high-pressure phases in MOOH (M = Al, Ga, In)
- Articles
- Nuwaite (Ni6GeS2) and butianite (Ni6SnS2), two new minerals from the Allende meteorite: Alteration products in the early solar system
- The role of magma mixing, identification of mafic magma inputs, and structure of the underlying magmatic system at Mount St. Helens
- Thermodynamic properties of natural melilites
- Thermal conductivity anomaly in spin-crossover ferropericlase under lower mantle conditions and implications for heat flow across the core-mantle boundary
- Electronic properties and compressional behavior of Fe–Si alloys at high pressure
- Diffusion of molybdenum and tungsten in anhydrous and hydrous granitic melts
- High-pressure single-crystal structural analysis of AlSiO3OH phase egg
- Structural variations along the apatite F-OH join
- Raman modes of carbonate minerals as pressure and temperature gauges up to 6 GPa and 500 °C
- Crystallization conditions of micas in oxidized igneous systems
- The role of crustal melting in the formation of rhyolites: Constraints from SIMS oxygen isotope data (Chon Aike Province, Patagonia, Argentina)
- New Mineral Names
- Book Review
Articles in the same Issue
- Letter
- Rapid solid-state sintering in volcanic systems
- How geometry and anisotropy affect residual strain in host-inclusion systems: Coupling experimental and numerical approaches
- Special collection: Earth analogs for martian geological materials and processes
- Diverse mineral assemblages of acidic alteration in the Rio Tinto area (southwest Spain): Implications for Mars
- Special collection: From magmas to ore deposits
- Archaean hydrothermal fluid modified zircons at Sunrise Dam and Kanowna Belle gold deposits, Western Australia: Implications for post-magmatic fluid activity and ore genesis
- Special collection: Water in nominally hydrous and anhydrous minerals
- New high-pressure phases in MOOH (M = Al, Ga, In)
- Articles
- Nuwaite (Ni6GeS2) and butianite (Ni6SnS2), two new minerals from the Allende meteorite: Alteration products in the early solar system
- The role of magma mixing, identification of mafic magma inputs, and structure of the underlying magmatic system at Mount St. Helens
- Thermodynamic properties of natural melilites
- Thermal conductivity anomaly in spin-crossover ferropericlase under lower mantle conditions and implications for heat flow across the core-mantle boundary
- Electronic properties and compressional behavior of Fe–Si alloys at high pressure
- Diffusion of molybdenum and tungsten in anhydrous and hydrous granitic melts
- High-pressure single-crystal structural analysis of AlSiO3OH phase egg
- Structural variations along the apatite F-OH join
- Raman modes of carbonate minerals as pressure and temperature gauges up to 6 GPa and 500 °C
- Crystallization conditions of micas in oxidized igneous systems
- The role of crustal melting in the formation of rhyolites: Constraints from SIMS oxygen isotope data (Chon Aike Province, Patagonia, Argentina)
- New Mineral Names
- Book Review