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The Origin and Evolution of Earth’s Deep Structure 地球深部结构的起源与演化
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-29 DOI: 10.1007/s10712-026-09932-z
Peng Wang
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引用次数: 0
The Footsteps of Research on Electrical Conductivity Distribution in Volcanically and Seismically Active Japan Arcs: Interpretation from the Perspective of Subduction Dynamics 日本火山和地震活动弧的电导率分布研究进展:俯冲动力学的解释
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-27 DOI: 10.1007/s10712-026-09929-8
Maki Hata
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引用次数: 0
Using Atmospheric Waves for the Detection and Early Warning of Natural Hazards: A Review Combining Results from the Neutral Atmosphere and the Ionosphere 利用大气波进行自然灾害的探测和预警:结合中性大气和电离层结果的综述
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-19 DOI: 10.1007/s10712-025-09909-4
Sabine Wüst, Marco Guerra, Jaroslav Chum, L. Claire Gasque
Waves transport energy through the atmosphere without transporting mass. Often excited in the troposphere, they can propagate horizontally and vertically over long distances, depending on the type of wave and the background atmosphere. The fastest atmospheric waves are (infra)sound and acoustic gravity waves. The list of possible reasons for the generation of these atmospheric waves is not short; here, we concentrate on natural hazards. Due to their comparatively high propagation speed, infrasound and acoustic gravity waves can contribute to or even improve early warning of natural hazards, even when measured at high altitudes. Traditionally, each scientific community—the one that deals with the neutral atmosphere and the one that addresses the ionosphere—usually works on its own. The aim of this manuscript is to bring together observations and results from both communities. The main challenges of the respective communities with regard to the use of these waves in the context of early warning of natural hazards are identified.
波在大气中传递能量而不传递质量。它们通常在对流层中被激发,根据波的类型和背景大气的不同,它们可以水平或垂直传播很远的距离。最快的大气波是(次)声和声重力波。产生这些大气波的可能原因并不短;在这里,我们专注于自然灾害。由于其相对较高的传播速度,次声和声重力波可以有助于甚至改善自然灾害的早期预警,即使在高海拔地区测量也是如此。传统上,每个科学团体——研究中性大气的和研究电离层的——通常都是各自为题。这份手稿的目的是汇集两个群体的观察和结果。确定了各自社区在自然灾害早期预警中使用这些波浪方面面临的主要挑战。
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引用次数: 0
Seismic Petrophysical Inversion Guided by Rock Physics Modeling for Quantitative Estimation of Permeability and Gas Saturation in Volcanic Reservoirs 以岩石物理建模为指导的地震岩石物理反演定量估计火山岩储层渗透率和含气饱和度
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-14 DOI: 10.1007/s10712-026-09930-1
Yuedong Li, Zhiqi Guo, Cai Liu
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引用次数: 0
Recent Advances in 2D Frequency-Domain Marine Controlled-Source EM Inversion Using Adjoint Approximate Sensitivities 基于伴随近似灵敏度的二维频域海洋可控源电磁反演研究进展
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-14 DOI: 10.1007/s10712-025-09925-4
Gang Li, Yutao Liu, Octavio Castillo-Reyes
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引用次数: 0
Filtering Unevenly Spaced Geophysical Time Series as an Ill-Posed Problem 非均匀间隔地球物理时间序列的不适定问题滤波
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-13 DOI: 10.1007/s10712-025-09924-5
Kunpu Ji, Lin Zhang, Fengwei Wang
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引用次数: 0
Slabs and Plumes Beneath South America Revealed by Whole-Mantle Tomography 全地幔层析成像揭示的南美洲板块和地幔柱
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-13 DOI: 10.1007/s10712-025-09926-3
Genti Toyokuni, Dapeng Zhao
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引用次数: 0
A Unified Framework for Trend Uncertainty Assessment in Climate Data Records: Demonstration on Global Mean Sea Level 气候资料记录趋势不确定性评估的统一框架:全球平均海平面的论证
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-12 DOI: 10.1007/s10712-025-09922-7
Kevin Gobron, Roland Hohensinn, Xavier Loizeau, Claire E. Bulgin, Christopher J. Merchant, Emma R. Woolliams, Maurice G. Cox, Wouter Dorigo, Thomas Howard, Mary Langsdale, Adam C. Povey, Michaël Ablain, Janusz Bogusz, Alexander Gruber, Anna Klos, Jonathan Mittaz
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引用次数: 0
Error Covariance Structure Caused by Uncertainties in Atmospheric Correction for Optical Sensors 光学传感器大气校正中不确定性引起的误差协方差结构
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-12 DOI: 10.1007/s10712-025-09921-8
Simon Blessing, Ralf Giering
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引用次数: 0
Unconventional Three-Dimensional Active Seismic Tomography Applied in the Lousal Mine (Iberian Pyrite Belt, Portugal) 非常规三维活动地震层析成像在葡萄牙伊比利亚黄铁矿带Lousal矿中的应用
IF 4.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2025-12-25 DOI: 10.1007/s10712-025-09920-9
Ines Hamak, Pedro Teixeira, José Borges, Ivan Koulakov, Rui Oliveira, Bento Caldeira, Mourad Bezzeghoud, João X. Matos, Sofia Andringa
The Lousal Mine (Iberian Pyrite Belt, Portugal) was operated from 1900 to 1988 for the extraction of massive sulphides and was later rehabilitated as a science museum. It was selected as a test site for underground muon tomography applied to geophysical surveys, as part of the LouMu project. This study focuses on seismic tomography to analyse the subsurface above the mine gallery, primarily surveyed by a muography telescope, which was developed specifically for this site by the Laboratory of Instrumentation and Experimental Particle Physics. To validate the muon tomography results, an initial approach using conventional 2D seismic refraction failed to reach the Waldemar gallery depth, due to limited seismic ray coverage. Therefore, an innovative setup using surface shots and in-gallery geophones was implemented, providing full ray coverage. A 3D velocity model was then produced using the ATOM3D code, which enabled the integration of this configuration and performed travel-time inversion for velocity calculation. A regional dextral strike-slip fault, the Corona Fault (CF), crosses the surveyed area, and served as the main focus of this investigation. The 3D velocity model successfully detected this structure, that corresponded to the boundary between positive anomalies of the Volcano-Sedimentary Complex (VSC) and negative anomalies of the Phyllite-Quartzite Group (PQG). The absolute velocity distribution showed a distinct offset around the Corona Fault (CF), indicating a dextral strike-slip mechanism. A subvertical extension of secondary faults was observed, reflecting deformation similar to that of the main tectonic context. Previous data from the gallery confirmed that these results are consistent with the known geology and can serve as a reference for the muon tomography interpretations.
卢萨尔矿(葡萄牙伊比利亚黄铁矿带)于1900年至1988年开采块状硫化物,后来恢复为科学博物馆。作为楼木工程的一部分,它被选为地下介子层析成像应用于地球物理调查的试验场。这项研究的重点是地震层析成像,以分析矿廊上方的地下,主要是通过仪器和实验粒子物理实验室专门为该地点开发的摄影望远镜进行调查。为了验证介子层析成像结果,由于地震射线覆盖范围有限,使用传统的二维地震折射的初始方法未能达到Waldemar走廊深度。因此,采用了表面拍摄和画廊内检波器的创新设置,提供了全射线覆盖。然后使用ATOM3D代码生成三维速度模型,该模型可以集成该配置,并对速度计算进行走时反演。一个区域右走滑断层,电晕断层(CF)穿过调查区域,成为本次调查的主要焦点。三维速度模型成功探测到该构造,该构造对应于火山-沉积杂岩(VSC)的正异常和千层岩-石英岩群(PQG)的负异常之间的边界。绝对速度分布在冕状断层周围有明显的偏移,表明其为右向走滑机制。观察到次级断裂的亚垂向伸展,反映了与主构造背景相似的变形。先前从画廊获得的数据证实,这些结果与已知的地质情况一致,可以作为介子断层扫描解释的参考。
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引用次数: 0
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Surveys in Geophysics
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