DiffSim: a user-friendly tool for precise magmatic timescale determination and error propagation via major element diffusion chronometry in magmatic phases

Eduardo Morgado, Daniel J. Morgan
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Abstract

Diffusion chronometry is a technique gaining interest in the scientific community related to volcanology and petrology; however, modelling can be challenging for non-expert users. Here, we present DiffSim, a user-friendly standalone freeware that allows users to calculate magmatic timescales simulating 1D diffusion of major elements in olivine, orthopyroxene, titanomagnetite, and melt (inclusions). The freeware works solving the Fick’s second law equation (for both Cartesian and spherical polar coordinates, depending on the phase) using finite differences through the Crank-Nicolson method. Users must specify the initial composition vs. distance profile, the time resolution, and the intensive conditions (such as temperature, pressure, and oxygen fugacity). For orthorhombic phases, such as olivine and orthopyroxene, users must also specify the plunge and the trend of the (001)-axis and the angle traverse of the 2D section being studied. The best-fitting profile, comparing the natural (measured) and the modelled (calculated) profiles, is obtained using the least-squares fitting method in accordance with the total time specified by the user for performing the diffusion modelling. To determine the uncertainties of the timescale calculation, DiffSim propagates errors based on the uncertainties associated with each intensive condition and the experimental diffusivity measurements. DiffSim is available as executable freeware, allowing researchers and students to use diffusion chronometry to elucidate information about crustal processes with ease and precision.
DiffSim:通过岩浆相中主要元素扩散计时法精确确定岩浆时间尺度和误差传播的用户友好型工具
扩散时间测定法是一种与火山学和岩石学有关的科学界越来越感兴趣的技术;然而,对于非专业用户来说,建模可能具有挑战性。在此,我们介绍 DiffSim,这是一款用户友好型独立免费软件,允许用户通过模拟橄榄石、正长石、榍石和熔体(包裹体)中主要元素的一维扩散来计算岩浆时标。该免费软件通过 Crank-Nicolson 方法使用有限差分法求解菲克第二定律方程(笛卡尔坐标和球极坐标,取决于相位)。用户必须指定初始成分与距离曲线、时间分辨率和强化条件(如温度、压力和氧富集度)。对于橄榄石和正霞石等正方体相,用户还必须指定所研究的二维截面的(001)轴和角度横截面的倾角和趋势。根据用户指定的执行扩散建模的总时间,使用最小二乘拟合方法,比较自然(测量)剖面和建模(计算)剖面,获得最佳拟合剖面。为了确定时间刻度计算的不确定性,DiffSim 会根据与每个强化条件和实验扩散率测量相关的不确定性传播误差。DiffSim 是可执行的免费软件,研究人员和学生可利用扩散计时法轻松、精确地阐明有关地壳过程的信息。
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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