WinMIgob: A Windows program for magnetite-ilmenite geothermometer and oxygen barometer

IF 1.1 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Journal of Geosciences Pub Date : 2021-04-07 DOI:10.3190/JGEOSCI.319
F. Yavuz
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引用次数: 6

Abstract

A Microsoft® Visual Basic software, called WinMIgob, has been developed for wet-chemical and electron-microprobe compositions of coexisting magnetite–ulvöspinel and ilmenite–hematite solid solutions to calculate the temperature (T, °C) and oxygen fugacity (fO2) conditions of magmatic and metamorphic rocks. The program allows the users to enter total of 34 input variables, including Sample No, SiO2, TiO2, Al2O3, V2O3, Cr2O3, Nb2O3, Fe2O3, FeO, MnO, NiO, ZnO, MgO, CaO, Na2O, K2O, BaO (wt. %) for each magnetite and ilmenite compositional data. WinMIgob enables to enter and load multiple magnetite and ilmenite analyses in the program’s data entry section. Alternatively, the composition of magnetite–ilmenite pairs can be typed in a blank Excel file as in the above order and then loaded into the program’s data entry screen for data processing. The ferric and ferrous iron contents from microprobe-derived total FeO (wt. %) of magnetite–ilmenite compositions are estimated by stoichiometric constraints based on three different approaches. Using the calculated multiple magnetite and ilmenite analyses, WinMIgob estimates molecular (%) and mole fractions of magnetite, uvöspinel, ilmenite and hematite amounts. The program evaluates fourteen magnetite–ilmenite geothermometers, thirteen oxygen barometers and six relative to the nickel–nickel oxide (NNO) buffer values based on the different calibrations with various calculation methods. WinMIgob also allows the users to check if their magnetite–ilmenite pairs taken from rocks are within or departure from the Bacon–Hirschmann Mg/Mn exchange equilibrium line ± 2σ level. This program generates and stores all the calculated results in the Microsoft Excel file (i.e., Output.xlsx), which can be displayed and processed by any other software for further data presentation and graphing purposes. The compiled program code is distributed as a self-extracting setup file, including a help file, test data files and graphic files, which are intended to produce a high-quality printout.
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WinMIgob:一个用于磁铁矿地温计和氧气气压计的Windows程序
开发了一款名为WinMIgob的Microsoft®Visual Basic软件,用于共存的磁铁矿-ulvö尖晶石和钛铁矿-赤铁矿固溶体的湿化学和电子探针组成,以计算岩浆岩和变质岩的温度(T,°C)和氧逸度(fO2)条件。该程序允许用户为每个磁铁矿和钛铁矿的成分数据输入总共34个输入变量,包括样品号、SiO2、TiO2、Al2O3、V2O3、Cr2O3、Nb2O3、Fe2O3、FeO、MnO、NiO、ZnO、MgO、CaO、Na2O、K2O、BaO(wt.%)。WinMIgob能够在程序的数据输入部分输入和加载多个磁铁矿和钛铁矿分析。或者,磁铁矿-钛铁矿对的组成可以按照上述顺序在空白Excel文件中键入,然后加载到程序的数据输入屏幕中进行数据处理。基于三种不同的方法,通过化学计量约束来估计磁铁矿-钛铁矿组成中微探针衍生的总FeO(wt.%)中的铁和亚铁含量。使用计算的多次磁铁矿和钛铁矿分析,WinMIgob估计了磁铁矿、紫外尖晶石、钛铁矿和赤铁矿的分子(%)和摩尔分数。该程序根据不同的校准和各种计算方法,评估了14个磁铁矿-钛铁矿地热计、13个氧气气压计和6个相对于镍-镍氧化物(NNO)缓冲值。WinMIgob还允许用户检查从岩石中提取的磁铁矿-钛铁矿对是否在Bacon–Hirschmann Mg/Mn交换平衡线±2σ水平之内或之外。该程序生成所有计算结果并将其存储在Microsoft Excel文件(即Output.xlsx)中,该文件可由任何其他软件显示和处理,以用于进一步的数据展示和绘图目的。编译后的程序代码作为自解压设置文件分发,包括帮助文件、测试数据文件和图形文件,旨在生成高质量的打印输出。
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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来源期刊
Journal of Geosciences
Journal of Geosciences GEOSCIENCES, MULTIDISCIPLINARY-MINERALOGY
CiteScore
2.30
自引率
7.10%
发文量
15
审稿时长
>12 weeks
期刊介绍: The Journal of Geosciences is an international peer-reviewed journal published by the Czech Geological Society with support from the Czech Geological Survey. It accepts high-quality original research or review papers dealing with all aspects of the nature and origin of igneous and metamorphic rocks. The Journal focuses, mainly but not exclusively, on: -Process-oriented regional studies of igneous and metamorphic complexes- Research in structural geology and tectonics- Igneous and metamorphic petrology- Mineral chemistry and mineralogy- Major- and trace-element geochemistry, isotope geochemistry- Dating igneous activity and metamorphic events- Experimental petrology and mineralogy- Theoretical models of igneous and metamorphic processes- Mineralizing processes and mineral deposits. All the papers are written in English, even though they may be accompanied by an additional Czech abstract. Each contribution is a subject to peer review by at least two independent reviewers, typically at least one from abroad. The Journal appears 2 to 4 times a year. Formally it is divided in annual volumes, each of them including 4 issues.
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