Home Physical Sciences Vestaite, (Ti4+Fe2+) Ti34+ O9, a new mineral in the shocked eucrite Northwest Africa 8003
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Vestaite, (Ti4+Fe2+) Ti34+ O9, a new mineral in the shocked eucrite Northwest Africa 8003

  • Run-Lian Pang , Dennis Harries , Kilian Pollok , Ai-Cheng Zhang EMAIL logo and Falko Langenhorst
Published/Copyright: August 28, 2018
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Abstract

Our investigations on the shocked eucrite Northwest Africa (NWA) 8003 revealed the occurrence of a new mineral, vestaite [IMA 2017-068; (Ti4+Fe2+) Ti34+ O9], This mineral coexists with corundum, ilmenite, and Al-Ti-rich pyroxene in shock melt pockets. It has an empirical chemical formula of ( Ti0.734+Fe0.632+ Al0.60Mn0.03Mg0.02Cr0.01) Ti34+ O9 and the monoclinic C2/c structure of schreyerite. The ideal vestaite structure can be considered as a modular structure with an alternate intergrowth of M3O5-type (M = Ti4+,Fe2+,Al) and Ti2O4-type slabs. Alternatively, it can also be envisaged as a crystallographic shear structure with periodically shearing of rutile or α-PbO2 units. Streaking and splitting of diffraction spots observed in selected-area electron diffraction patterns indicate planar defects in the modular structure of vestaite. Our observations reveal that vestaite crystallized at high pressure (≤10 GPa) from a melt that represents a mixture of ilmenite and silicate components. A robust constraint on its formation conditions and stability field cannot yet be provided due to the lack of experimental data for these systems. Vestaite is a new, shock-generated mineral first found in a meteorite of the howardite- eucrite-diogenite (HED) clan, the largest achondrite group. Its discovery is not only of significance to the meteoritic mineralogy, but it could also be of interest to materials science.

Acknowledgments

This work was supported by the National Natural Science Foundation of China (Grant 41673068), the Natural Science Foundation of Jiangsu Province of China (Grant BK20170017), and the Gottfried Wilhelm Leibniz program of the Deutsche Forschungsgemeinschaft (LA830/14-1). Li-Xin Gu, Agnese Fazio, and Jia-Ni Chen are appreciated for their technical assistance in preparing FIB foils, SEM, and TEM observations. The first author is also grateful to the China Scholarship Council for a 2 year Ph.D. grant and to the group of Analytical Mineralogy of Micro- and Nanostructures, Friedrich Schiller University Jena for hosting her during this period. We thank Chi Ma and Erin Walton for their helpful reviews that improved the quality of the paper, and associate editor Steve Simon for his comments and editorial handling.

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Received: 2018-02-23
Accepted: 2018-05-25
Published Online: 2018-08-28
Published in Print: 2018-09-25

© 2018 Walter de Gruyter GmbH, Berlin/Boston

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