矿物晶体学：X. 碳酸盐

IF 0.6 4区材料科学 Q4 CRYSTALLOGRAPHY

Crystallography Reports Pub Date : 2024-03-19 DOI:10.1134/S1063774523601569

D. Yu. Pushcharovsky

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引用次数: 0

摘要

碳酸盐类矿物占地球沉积外壳的 18%，即地壳质量的 1.7%。碳酸盐是海洋沉积物的主要矿物。这是一类分布广泛但晶体化学研究不足的矿物，包括 290 个种类。在 90 种无水碳酸盐中，可分为两大类，包括斜方体和正方体对称的矿物，它们积累了地壳中 90% 的碳。本文探讨了这两大类的主要代表矿物和其他常见碳酸盐的结构特征。报告了碳酸盐在深层地球圈中可能发生的转化数据。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

Mineralogical Crystallography: X. Carbonates

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Mineralogical Crystallography: X. Carbonates

The minerals belonging to the class of carbonates constitute 18% of the Earth’s sedimentary shell, which is 1.7 wt % of the Earth’s crust mass. Carbonates are the main minerals of marine sediments. This is a widespread but crystallochemically understudied class of minerals, which includes 290 species. Among the 90 anhydrous carbonates, two large groups are distinguished, which include minerals with rhombohedral and orthorhombic symmetries, accumulating 90% of carbon of the Earth’s crust. The characteristic structural features of the main representatives of these groups and other common carbonates are considered. Data on possible transformations of carbonates in deep geospheres are reported.

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来源期刊

Crystallography Reports 化学-晶体学

CiteScore

1.10

自引率

28.60%

发文量

审稿时长

4-8 weeks

期刊介绍： Crystallography Reports is a journal that publishes original articles short communications, and reviews on various aspects of crystallography: diffraction and scattering of X-rays, electrons, and neutrons, determination of crystal structure of inorganic and organic substances, including proteins and other biological substances; UV-VIS and IR spectroscopy; growth, imperfect structure and physical properties of crystals; thin films, liquid crystals, nanomaterials, partially disordered systems, and the methods of studies.