白钨矿与HCl溶液在400和500℃，100 MPa和不同f(O2)下的相互作用特征的勘误(根据实验和计算数据)

IF 0.8 4区地球科学 Q3 GEOLOGY

Geology of Ore Deposits Pub Date : 2023-09-18 DOI:10.1134/s1075701523360011

A. F. Redkin, N. P. Kotova

引用次数: 0

摘要

本文的勘误表已发表:https://doi.org/10.1134/S1075701523360011

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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Erratum to: Features of the Interaction of Scheelite with HCl Solutions at 400 and 500°C, 100 MPa, and Various f(O2) (According to Experimental and Calculated Data)

An Erratum to this paper has been published: https://doi.org/10.1134/S1075701523360011

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来源期刊

Geology of Ore Deposits 地学-地质学

CiteScore

1.10

自引率

14.30%

发文量

审稿时长

6-12 weeks

期刊介绍： Geology of Ore Deposits is a periodical covering the topic of metallic and nonmetallic mineral deposits, their formation conditions, and spatial and temporal distribution. The journal publishes original scientific articles and reviews on a wide range of problems in theoretical and applied geology. The journal focuses on the following problems: deep geological structure and geodynamic environment of ore formation; distribution pattern of metallogenic zones and mineral deposits; geology and formation environment of large and unique metallic and nonmetallic deposits; mineralogy of metallic and nonmetallic deposits; physicochemical and isotopic characteristics and geochemical environment of ore deposition; evolution of ore-forming systems; radiogeology and radioecology, economic problems in exploring, developing, and mining of ore commodities.