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Structure of type A CAI-like melts: A view from multi-nuclear NMR study of melilite (Ca2Al2SiO7-Ca2MgSi2O7) glasses

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Title
Structure of type A CAI-like melts: A view from multi-nuclear NMR study of melilite (Ca2Al2SiO7-Ca2MgSi2O7) glasses
Other Titles
운석내 태양계 최초 물질(CAI) 조성의 멜트 구조: 멜릴라이트 글래스의 NMR 연구의 시사점
Authors
Park, Sun Young
Park, Changkun
Kim, Hyun Na
Lee, Seoyoung
Lee, Sung Keun
Subject
Geochemistry & Geophysics
Keywords
Melilite glasses and melts; Structure and disorder; High-resolution solid-state nuclear magnetic; resonance; Viscosity and diffusivity
Issue Date
2020-12
Citation
Park, Sun Young, et al. 2020. "Structure of type A CAI-like melts: A view from multi-nuclear NMR study of melilite (Ca2Al2SiO7-Ca2MgSi2O7) glasses". CHEMICAL GEOLOGY, 558(1): 119894-119903.
Abstract
Exploring the polymerization and structural disorder of Ca-Al-rich inclusion (CAI)-like melts is a key question in cosmochemistry due to strong implications for macroscopic properties of melts (i.e., viscosity and diffusivity). Here, we report experimental results showing the effect of composition on the structure of melilite glasses and melts [akermanite (Ak, Ca2MgSi2O7) - gehlenite (Gh, Ca2Al2SiO7)] in type A CAIs with varying composition using high-resolution solid-state nuclear magnetic resonance (NMR). The 27Al magic angle spinning (MAS) and 3Q (triple quantum) MAS NMR spectra of melilite glasses show predominant [4]Al. A non-negligible fraction of [5]Al is observed in Ak50Gh50 and Ak72Gh28 glasses and it slightly increases with increasing akermanite content. The 17O 3QMAS NMR spectra of melilite glasses show that bridging oxygens (BOs, Si-O-Si, Al-O-Al, and Si-O-Al) and non-bridging oxygens (NBOs, Ca-O-Si, Ca-O-Al, and mixed {Ca, Mg}-NBO) are partially resolved. Despite the strong preference of Si over Al for NBOs, for the first time, Ca-O-Al is observed in natural melts (i.e., gehlenite and Ak25Gh75 glasses and melts). The results show that Al-NBO (~150 ppm in MAS dimension) can be distinguished from Si-NBO (~110 ppm) in melilite glasses and melts. The fraction of NBO increases with increasing akermanite content. The experimental results suggest that compositioninduced structural changes should be considered to interpret the melt viscosity, diffusivity, and oxygen isotopic composition of CAI-like melts in the early Solar System.
URI
https://repository.kopri.re.kr/handle/201206/11962
DOI
http://dx.doi.org/10.1016/j.chemgeo.2020.119894
Appears in Collections  
2020-2020, Antarctic geology and meteorite research based on the Jangbogo station: Crustal evolution of Victoria Land and characteristics of asteroidal materials (20-20) / Lee, Mi Jung (PE20200)
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