Combining 3-D Probabilistic Kinematic Modeling With Thermal Resetting Measurements: An Approach to Reduce Uncertainty in Exhumation Histories

IF 2.9 2区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Sofia Brisson, Denise Degen, David Nathan, Florian Wellmann, Christoph von Hagke
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Abstract

To understand the exhumation history of orogens and their fold-thrust belts, it is important to accurately reconstruct their time-temperature evolution. This is often done by employing thermokinematic models. One problem of current approaches is that they are limited in prescribing geometric constraints only as far as they affect transient thermal conditions. This often results in 2-D plane strain assumptions, and a simple treatment of structural and kinematic uncertainties. In this work, we combine 3-D kinematic forward modeling with a random sampling approach to automatically generate an ensemble of kinematic models in the range of assigned geometric uncertainties. Using Markov Chain Monte Carlo, each randomly generated model is assessed regarding how well it fits the available paleo-depth data taken from low-temperature thermochronology. The resulting, more robust model can then be used to re-interpret the thermal resetting data. We first apply this method to synthetic experiments with variable structural complexity and sample uncertainties, and later to the Alpine fold-thrust belt, the Subalpine Molasse. Results show that it is possible to use thermochronological data to make predictions about exhumation, which can be translated into likelihood functions to obtain the range of 3-D kinematic forward models explaining the data. Though the method performs well for the synthetic models, additional thermochronological parameters may need to be considered to improve the inversion results for structurally complex settings. The method is useful, however, to study alternative mechanisms of exhumation for the thermochronological samples that are not respected by the modeling, even when uncertainty is considered.

Abstract Image

结合三维概率运动学建模与热复位测量:一种减少挖掘历史不确定性的方法
为了了解造山带及其褶皱冲断带的发掘历史,准确地重建造山带的时温演化是十分重要的。这通常是通过采用热力学模型来完成的。当前方法的一个问题是,它们在规定几何约束方面受到限制,只有当它们影响瞬态热条件时。这通常导致二维平面应变假设,以及对结构和运动不确定性的简单处理。在这项工作中,我们将三维运动学正演建模与随机抽样方法相结合,在指定的几何不确定性范围内自动生成运动学模型集合。使用马尔科夫链蒙特卡罗,评估每个随机生成的模型是否适合从低温热年代学中获得的可用古深度数据。由此产生的更稳健的模型可以用来重新解释热重置数据。我们首先将该方法应用于具有可变结构复杂性和样品不确定性的综合实验,然后应用于高山褶皱冲断带亚高山Molasse。结果表明,利用热年代学数据对挖掘进行预测是可行的,这些预测可以转化为似然函数,从而获得解释数据的三维运动学正演模型的范围。虽然该方法在合成模型中表现良好,但对于结构复杂的环境,可能需要考虑额外的热时间参数来改善反演结果。然而,该方法对于研究模型未考虑的热年代学样品的挖掘替代机制是有用的,即使考虑了不确定性。
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来源期刊
Geochemistry Geophysics Geosystems
Geochemistry Geophysics Geosystems 地学-地球化学与地球物理
CiteScore
5.90
自引率
11.40%
发文量
252
审稿时长
1 months
期刊介绍: Geochemistry, Geophysics, Geosystems (G3) publishes research papers on Earth and planetary processes with a focus on understanding the Earth as a system. Observational, experimental, and theoretical investigations of the solid Earth, hydrosphere, atmosphere, biosphere, and solar system at all spatial and temporal scales are welcome. Articles should be of broad interest, and interdisciplinary approaches are encouraged. Areas of interest for this peer-reviewed journal include, but are not limited to: The physics and chemistry of the Earth, including its structure, composition, physical properties, dynamics, and evolution Principles and applications of geochemical proxies to studies of Earth history The physical properties, composition, and temporal evolution of the Earth''s major reservoirs and the coupling between them The dynamics of geochemical and biogeochemical cycles at all spatial and temporal scales Physical and cosmochemical constraints on the composition, origin, and evolution of the Earth and other terrestrial planets The chemistry and physics of solar system materials that are relevant to the formation, evolution, and current state of the Earth and the planets Advances in modeling, observation, and experimentation that are of widespread interest in the geosciences.
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