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LitMod3D : an interactive 3-D software to model the thermal, compositional, density, seismological, and rheological structure of the lithosphere and sublithospheric upper mantle

机译:LitMod3D:一种交互式3-D软件,可对岩石圈和岩石圈下上地幔的热,成分,密度,地震和流变结构进行建模

摘要

We present an interactive 3-D computer program (LitMod3D) developed to perform combined geophysical-petrological modeling of the lithosphere and sublithospheric upper mantle. In contrast to other available modeling software, LitMod3D is built within an internally consistent thermodynamic-geophysical framework, where all relevant properties are functions of temperature, pressure, and composition. By simultaneously solving the heat transfer, thermodynamic, rheological, geopotential, and isostasy (local and flexural) equations, the program outputs temperature, pressure, surface heat flow, density (bulk and single phase), seismic wave velocities, geoid and gravity anomalies, elevation, and lithospheric strength for any given model. These outputs can be used to obtain thermal and compositional models of the lithosphere and sublithospheric upper mantle that simultaneously fit all available geophysical and petrological observables. We illustrate some of the advantages and limitations of LitMod3D using synthetic models and comparing our predictions with those from other modeling methods. In particular, we show that (1) temperature at midlithosphere depths may be overestimated by as much as 200 K when compositional heterogeneities in the mantle and T-P effects are not considered in lithospheric models and (2) the neglect of mantle phase transformations on gravity-based models in thin-crust settings can result in a significant overestimation and underestimation of the derived crustal thickness and its internal density distribution, respectively.
机译:我们提出了一个交互式的3-D计算机程序(LitMod3D),该程序开发用于执行岩石圈和岩石圈下上地幔的组合地球物理-岩石学建模。与其他可用的建模软件相比,LitMod3D构建在内部一致的热力学-地球物理框架内,其中所有相关属性都是温度,压力和成分的函数。通过同时求解热传递,热力学,流变学,地势和等渗(局部和挠曲)方程,该程序输出温度,压力,表面热流,密度(体相和单相),地震波速度,大地水准面和重力异常,高度,以及任何给定模型的岩石圈强度。这些输出可用于获取岩石圈和岩石圈下上地幔的热模型和成分模型,这些模型同时适合所有可用的地球物理和岩石学观测资料。我们使用合成模型来说明LitMod3D的一些优点和局限性,并将我们的预测与其他建模方法的预测进行比较。特别是,我们表明(1)如果在岩石圈模型中未考虑地幔中的成分非均质性和TP效应,则岩石圈中层深度的温度可能被高估了200 K,并且(2)忽略了重力作用下的地幔相变。薄壳环境中基于模型的模型可能分别导致对得出的地壳厚度及其内部密度分布的明显高估和低估。

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