Moho depth model of South America from a machine learning approach

IF 1.7 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Marcus Vinicius Aparecido Gomes de Lima , Italo Gomes Gonçalves , José Eduardo Pereira Soares , Randell Alexander Stephenson
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Abstract

Crustal structure models play an important role in the characterization of seismogenic zones, in the regional delimitation of geological provinces and particularly, in understanding the genesis and evolution of sedimentary basins. Despite the increasing number of new seismic surveys and seismographic networks in South America, crustal thickness measurements are still scarce and irregularly sampled, reducing the resolution of crustal model maps. To overcome these challenges, a novel approach based on machine learning techniques is proposed, in order to explore higher resolution gravity datasets in the interpolation of crustal thickness measurement points obtained from previous seismic/seismological compilations. The algorithm used in this study is based on Gaussian processes prediction methods, which allowed inferring the depth of Moho to South America. The prediction error of the model obtained from the training and testing database was 3.48 km, which is compatible with the uncertainties derived from the H-k stacking analysis. The depth range varied from 69.8 km beneath the Andes to 4.3 km in oceanic regions. The average Moho depth for the South American Platform is 39.1 km, allowing a spatial correlation of deeper and shallower Moho regions with different types of continental basins. Compared to other models, the model resulting from this study presents fine-scale features highlighting the limits of the main tectonic domains and a good agreement with the suture zones. Overall, this study demonstrates the potential of applying machine learning tools in crustal-scale imaging using sparse datasets, providing new advances in Moho modeling of the South America, as well as new perspectives on its the history and tectonic evolution.

从机器学习方法看南美洲莫霍水深模型
地壳结构模型在确定地震带的特征、划分地质省的区域范围,特别是在了解沉积盆地的成因和演化方面发挥着重要作用。尽管南美洲新的地震勘探和地震学网络不断增加,但地壳厚度测量仍然很少,而且采样不规则,降低了地壳模型图的分辨率。为了克服这些挑战,提出了一种基于机器学习技术的新方法,以便在对以前地震/地震学汇编获得的地壳厚度测量点进行插值时,探索更高分辨率的重力数据集。本研究中使用的算法基于高斯过程预测方法,可以推断南美洲莫霍深度。从训练和测试数据库中获得的模型预测误差为 3.48 千米,与 H-k 叠加分析得出的不确定性相符。深度范围从安第斯山脉下的 69.8 千米到海洋地区的 4.3 千米不等。南美地台的平均莫霍深度为 39.1 千米,这使得较深和较浅的莫霍区域与不同类型的大陆盆地在空间上相互关联。与其他模型相比,本研究得出的模型呈现出精细的尺度特征,突出了主要构造域的界限,并与缝合带很好地吻合。总之,这项研究展示了利用稀疏数据集在地壳尺度成像中应用机器学习工具的潜力,为南美洲莫霍模型的建立提供了新的进展,也为南美洲的历史和构造演化提供了新的视角。
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来源期刊
Journal of South American Earth Sciences
Journal of South American Earth Sciences 地学-地球科学综合
CiteScore
3.70
自引率
22.20%
发文量
364
审稿时长
6-12 weeks
期刊介绍: Papers must have a regional appeal and should present work of more than local significance. Research papers dealing with the regional geology of South American cratons and mobile belts, within the following research fields: -Economic geology, metallogenesis and hydrocarbon genesis and reservoirs. -Geophysics, geochemistry, volcanology, igneous and metamorphic petrology. -Tectonics, neo- and seismotectonics and geodynamic modeling. -Geomorphology, geological hazards, environmental geology, climate change in America and Antarctica, and soil research. -Stratigraphy, sedimentology, structure and basin evolution. -Paleontology, paleoecology, paleoclimatology and Quaternary geology. New developments in already established regional projects and new initiatives dealing with the geology of the continent will be summarized and presented on a regular basis. Short notes, discussions, book reviews and conference and workshop reports will also be included when relevant.
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