An example of high-T, high-symmetry crystallization: Spherical (Mg,Fe)-oxides formed by particle attachment in the shocked martian meteorite Northwest Africa 7755
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Ai-Cheng Zhang
, Shu-Zhou Wang
, Naotaka Tomioka , Xian-Cai Lu , Zhi-Yuan Ding , Chi Ma , Peng Wang , Jia-Ni Chen , Sheng Xu , Li-Xin Gu , Yuan-Qiang Bai , Yang Li , Naoya Sakamoto and Ru-Cheng Wang
Abstract
Crystallization is one of the most fundamental processes for both solid inorganic and organic materials in nature. The classical crystallization model mainly involves the monomer-by-monomer addition of simple chemical species. Recently, nanoparticle attachment has been realized as an important mechanism of crystallization in comparatively low-temperature aqueous natural and synthetic systems. However, no evidence of crystallization by particle attachment has been reported in petrologically important melts. In this study, we described spherical (Mg,Fe)-oxides with a protrusion surface in a shock-induced melt pocket from the martian meteorite Northwest Africa 7755. Transmission electron microscopic observations demonstrate that the (Mg,Fe)-oxides are structure-coherent intergrowth of ferropericlase and magnesioferrite. The magnesioferrite is mainly present adjacent to the interface between (Mg,Fe)-oxides spherules and surrounding silicate glass, but not in direct contact with the silicate glass. Thermodynamic and kinetic considerations suggest that development of the spherical (Mg,Fe)-oxides can be best interpreted with crystallization by particle attachment and subsequent Ostwald ripening. This indicates that crystallization by particle attachment can also take place in high-temperature melts and has potential implications for understanding the nucleation and growth of early-stage crystals in high-temperature melts, such as chondrules in the solar nebula, erupted volcanic melts, and probably even intrusive magmas.
Funding
This work was financially supported by Natural Science Foundations of China (grant 41673068) and Jiangsu Province of China (grant BK20170017).
Acknowledgments
We thank two anonymous reviewers for their helpful comments and Associate Editor Bruce Watson for his editorial efforts.
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© 2019 Walter de Gruyter GmbH, Berlin/Boston
Articles in the same Issue
- Highlights and Breakthroughs
- Iron carbide in the core
- Reconstruction of residual melts from the zeolitized explosive products of alkaline-mafic volcanoes
- Inefficient high-temperature metamorphism in orthogneiss
- Nitrogen incorporation in silicates and metals: Results from SIMS, EPMA, FTIR, and laser-extraction mass spectrometry
- Activation of [100](001) slip system by water incorporation in olivine and the cause of seismic anisotropy decrease with depth in the asthenosphere
- In-situ high-temperature vibrational spectra for synthetic and natural clinohumite: Implications for dense hydrous magnesium silicates in subduction zones
- Stability of the hydrous phases of Al-rich phase D and Al-rich phase H in deep subducted oceanic crust
- Minerals in cement chemistry: A single-crystal neutron diffraction study of ettringite, Ca6Al2(SO4)3(OH)12·27H2O
- Nature of hydrogen defects in clinopyroxenes from room temperature up to 1000 °C: Implication for the preservation of hydrogen in the upper mantle and impact on electrical conductivity
- Phase transition boundary between fcc and hcp structures in Fe-Si alloy and its implications for terrestrial planetary cores
- Cathodoluminescence features, trace elements, and oxygen isotopes of quartz in unidirectional solidification textures from the Sn-mineralized Heemskirk Granite, western Tasmania
- Controls on cassiterite (SnO2) crystallization: Evidence from cathodoluminescence, trace-element chemistry, and geochronology at the Gejiu Tin District
- Anomalous elastic behavior of phase egg, AlSiO3(OH), at high pressures
- “Kamchatite” diamond aggregate from northern Kamchatka, Russia: New find of diamond formed by gas phase condensation or chemical vapor deposition
- An example of high-T, high-symmetry crystallization: Spherical (Mg,Fe)-oxides formed by particle attachment in the shocked martian meteorite Northwest Africa 7755
- Letter
- Zinc transport in hydrothermal fluids: On the roles of pressure and sulfur vs. chlorine complexing
- Book Review
- Book Review: Infrared and Raman Spectroscopies of Clay Minerals
Articles in the same Issue
- Highlights and Breakthroughs
- Iron carbide in the core
- Reconstruction of residual melts from the zeolitized explosive products of alkaline-mafic volcanoes
- Inefficient high-temperature metamorphism in orthogneiss
- Nitrogen incorporation in silicates and metals: Results from SIMS, EPMA, FTIR, and laser-extraction mass spectrometry
- Activation of [100](001) slip system by water incorporation in olivine and the cause of seismic anisotropy decrease with depth in the asthenosphere
- In-situ high-temperature vibrational spectra for synthetic and natural clinohumite: Implications for dense hydrous magnesium silicates in subduction zones
- Stability of the hydrous phases of Al-rich phase D and Al-rich phase H in deep subducted oceanic crust
- Minerals in cement chemistry: A single-crystal neutron diffraction study of ettringite, Ca6Al2(SO4)3(OH)12·27H2O
- Nature of hydrogen defects in clinopyroxenes from room temperature up to 1000 °C: Implication for the preservation of hydrogen in the upper mantle and impact on electrical conductivity
- Phase transition boundary between fcc and hcp structures in Fe-Si alloy and its implications for terrestrial planetary cores
- Cathodoluminescence features, trace elements, and oxygen isotopes of quartz in unidirectional solidification textures from the Sn-mineralized Heemskirk Granite, western Tasmania
- Controls on cassiterite (SnO2) crystallization: Evidence from cathodoluminescence, trace-element chemistry, and geochronology at the Gejiu Tin District
- Anomalous elastic behavior of phase egg, AlSiO3(OH), at high pressures
- “Kamchatite” diamond aggregate from northern Kamchatka, Russia: New find of diamond formed by gas phase condensation or chemical vapor deposition
- An example of high-T, high-symmetry crystallization: Spherical (Mg,Fe)-oxides formed by particle attachment in the shocked martian meteorite Northwest Africa 7755
- Letter
- Zinc transport in hydrothermal fluids: On the roles of pressure and sulfur vs. chlorine complexing
- Book Review
- Book Review: Infrared and Raman Spectroscopies of Clay Minerals