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Periodic and non-periodic stacking in molybdenite (MoS2) revealed by STEM

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Published/Copyright: May 27, 2022
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Abstract

Polytypism is a typical feature of layered minerals with differences only in stacking sequences. There is no obvious “phase” boundary among different polytypes, although the frequency of polytypes occurrence is related to its crystallization environment. In the past decades, X‑ray studies of molybdenite specimens from a variety of geological environments have revealed that most molybdenite crystals contain both 2H1 (hexagonal) and 3R (rhombohedral) polytypes. However, the stacking sequences of these molybdenite polytypic intergrowths and their formation mechanism are not well understood. Here, we report stacking faults and domains of long-period polytypes identified by high-angle annular dark-field scanning transmission electron microscopy (HAADF-STEM) in a molybdenite sample from a carbonatite vein in the Huanglongpu Mo-Pb ore deposit in Qinling orogenic belt, Northern China. Several layers of disordered domains intergrown with ordered 2H1 domain were recognized based on the contrast in HAADF image with one-dimensional lattice fringes. In addition, a 30-layer long-period polytype was unambiguously identified by a STEM image. The stacking sequences of 4-, 6-, and 8-layer disordered domains and the 30-layer long-period polytype were further examined using HRSTEM images at the atomic resolution. A 2H3 polytype with three repetitions was also discovered in the sample. We propose that non-equilibrium conditions related to the fluctuation of fluid composition during crystallization resulted in the oscillation of 2H1 and 3R polytypes and intergrowth of various disordered domains. More broadly, our study demonstrates that HAADF-STEM imaging method may be applicable for studying other disordered layered crystals and twinned minerals.


‡ Special collection papers can be found online at http://www.minsocam.org/MSA/AmMin/special-collections.html.


Acknowledgments and Funding

The authors thank Daniel Hummer for handling this paper, and two anonymous reviewer for reviewing the manuscript and providing constructive comments and suggestions. This study was financially supported by the National Key R&D Program of China (2018YFA0702600), China National Funds for Distinguished Young Scientists (Grant No. 41825003), National Natural Science Foundation of China (Grant Nos. 41772039 and 41921003), Youth Innovation Promotion Association CAS (Grant No. 2021353), CAS Key Research Program of Frontier Sciences (Grant No. QYZDJ-SSW-DQC023), Tuguangchi Award for Excellent Young Scholar GIG, CAS, and Science and Technology Planning of Guangdong Province, China (2020B1212060055). This is Contribution No. IS-3170 from GIG-CAS.

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Received: 2021-02-16
Accepted: 2021-06-23
Published Online: 2022-05-27
Published in Print: 2022-05-27

© 2022 Mineralogical Society of America

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