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Structural hydroxyl distribution in jadeite grains and the diagenesis mechanism of jadeitite in Myanmar, Guatemala and Russia by Xing Yingying; Qi Lijian is a Engineering article available to read on EtoBox.

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## Materials Testing water, etc. [1]. The forms of water in the crust are stratified, and the upper crust is in the form of free water, as shown by Smithson et al. [2] and Zharikov et al. [3], the middle crust (dominated by feldspar rocks) and the lower crust (dominated by granulite) are mostly in the form of structural water [4][5][6][7] the Republic of Kazakhstan and the two sides of the Motagua fault in Guatemala. Jadeitite with a commercial exploitation value is mainly from Parkhan. Previous studies have shown that water exists in minerals in forms that include free water, fluid inclusion water, crystalline water, and structural There are few known jadeitite producing areas in the world, and these can be found in the Parkhan jadeitite belt (including Longkin and Tawmaw) in northwest Myanmar, Kotaki and Oo sacho in Japan, San Benito in California, USA, the Polar Urals and PayYer in Russia, the north part of Near Balkash in Carrying out jadeitite diagenesis in its basic state as well as in combination with the multiple fluid activities of water, we focused on jadeite grains in production areas such as Myanmar, Guatemala and Russia to determinethe essence of nominal anhydrous jade

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It is typically read by researchers, students, and practitioners in Engineering.

Author
Xing Yingying; Qi Lijian
Publisher
Walter de Gruyter GmbH
Published
2021
Language
EN
Field
Engineering (Physical Sciences)

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