Bayesian Preprocessing for Palaeomagnetic Sediment Records Using a Flexible Lock-In Function Approach

IF 3.9 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
L. Bohsung, M. Schanner, M. Korte, M. Holschneider
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引用次数: 0

Abstract

Geomagnetic field models covering past millennia rely on two main data sources: archaeomagnetic data, that provide snapshots of the geomagnetic field at specific locations, and sediment records, that deliver time series of the geomagnetic field from individual cores. The limited temporal and spatial global coverage with archaeomagnetic data necessitates use of sediment data, especially when models go further back in time. However, the accurate preprocessing and interpretation of sediment data is crucial. Unlike archaeomagnetic data, sediment data does not provide absolute values for intensities and declinations; instead, it represents relative variations. The detrital remanent magnetization (DRM) of sediment records is influenced by various depositional (dDRM) effects that can result in inclination shallowing, as well as post-depositional (pDRM) processes that cause a delayed and smoothed signal. To address the distortion associated with the pDRM effects, a novel class of flexible parameterized lock-in functions has been proposed. These lock-in functions involve four parameters, which are estimated using a Bayesian modeling technique and archaeomagnetic data. By extending the space of hyperparameters to include the calibration factor for intensities, the declination offsets and the inclination shallowing factor, we present a fully Bayesian preprocessing method for sediment records in form of a Python package, called sedprep. By applying the estimated parameters to the raw sediment data sedprep is able to provide a calibrated and preprocessed palaeomagnetic record.
基于弹性锁定函数的古地磁沉积记录贝叶斯预处理
覆盖过去几千年的地磁场模型依赖于两个主要的数据来源:考古磁场数据,提供了特定地点地磁场的快照;沉积物记录,提供了来自单个岩心的地磁场的时间序列。由于古磁数据覆盖的时间和空间有限,因此必须使用沉积物数据,特别是当模型追溯到更早的时候。然而,准确的预处理和解释沉积物数据是至关重要的。与古地磁数据不同,沉积物数据不能提供强度和赤纬的绝对值;相反,它代表了相对的变化。沉积记录的碎屑残余磁化(DRM)受到多种沉积(dDRM)效应的影响,这些沉积(dDRM)效应会导致倾斜变浅,而沉积后(pDRM)过程会导致信号的延迟和平滑。为了解决与pDRM效应相关的失真问题,提出了一类新的柔性参数化锁定函数。这些锁定函数涉及四个参数,这些参数是使用贝叶斯建模技术和考古磁数据估计的。通过扩展超参数的空间以包括强度的校准因子、偏角偏移量和倾角变浅因子,我们提出了一种以Python包形式的沉积物记录的完全贝叶斯预处理方法,称为sedprep。通过将估计参数应用于原始沉积物数据,sedprep能够提供校准和预处理的古地磁记录。
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来源期刊
Journal of Geophysical Research: Solid Earth
Journal of Geophysical Research: Solid Earth Earth and Planetary Sciences-Geophysics
CiteScore
7.50
自引率
15.40%
发文量
559
期刊介绍: The Journal of Geophysical Research: Solid Earth serves as the premier publication for the breadth of solid Earth geophysics including (in alphabetical order): electromagnetic methods; exploration geophysics; geodesy and gravity; geodynamics, rheology, and plate kinematics; geomagnetism and paleomagnetism; hydrogeophysics; Instruments, techniques, and models; solid Earth interactions with the cryosphere, atmosphere, oceans, and climate; marine geology and geophysics; natural and anthropogenic hazards; near surface geophysics; petrology, geochemistry, and mineralogy; planet Earth physics and chemistry; rock mechanics and deformation; seismology; tectonophysics; and volcanology. JGR: Solid Earth has long distinguished itself as the venue for publication of Research Articles backed solidly by data and as well as presenting theoretical and numerical developments with broad applications. Research Articles published in JGR: Solid Earth have had long-term impacts in their fields. JGR: Solid Earth provides a venue for special issues and special themes based on conferences, workshops, and community initiatives. JGR: Solid Earth also publishes Commentaries on research and emerging trends in the field; these are commissioned by the editors, and suggestion are welcome.
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