3D Cosmic Ray Muon Tomography from an Underground Tunnel
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作者:
Elena Guardincerri
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机构:Los Alamos National Laboratory,Department of Physics and Astronomy
Elena Guardincerri
Charlotte Rowe
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机构:Los Alamos National Laboratory,Department of Physics and Astronomy
Charlotte Rowe
Emily Schultz-Fellenz
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机构:Los Alamos National Laboratory,Department of Physics and Astronomy
Emily Schultz-Fellenz
Mousumi Roy
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机构:Los Alamos National Laboratory,Department of Physics and Astronomy
Mousumi Roy
Nicolas George
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机构:Los Alamos National Laboratory,Department of Physics and Astronomy
Nicolas George
Christopher Morris
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机构:Los Alamos National Laboratory,Department of Physics and Astronomy
Christopher Morris
Jeffrey Bacon
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机构:Los Alamos National Laboratory,Department of Physics and Astronomy
Jeffrey Bacon
Matthew Durham
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机构:Los Alamos National Laboratory,Department of Physics and Astronomy
Matthew Durham
Deborah Morley
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机构:Los Alamos National Laboratory,Department of Physics and Astronomy
Deborah Morley
Kenie Plaud-Ramos
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机构:Los Alamos National Laboratory,Department of Physics and Astronomy
Kenie Plaud-Ramos
Daniel Poulson
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机构:Los Alamos National Laboratory,Department of Physics and Astronomy
Daniel Poulson
Diane Baker
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机构:Los Alamos National Laboratory,Department of Physics and Astronomy
Diane Baker
Alain Bonneville
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机构:Los Alamos National Laboratory,Department of Physics and Astronomy
Alain Bonneville
Richard Kouzes
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机构:Los Alamos National Laboratory,Department of Physics and Astronomy
Richard Kouzes
机构:
[1] Los Alamos National Laboratory,Department of Physics and Astronomy
[2] University of New Mexico,undefined
[3] Pacific Northwest National Laboratory,undefined
来源:
Pure and Applied Geophysics
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2017年
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174卷
关键词:
Cosmic ray muons;
3-D inversion;
density tomography;
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摘要:
We present an underground cosmic ray muon tomographic experiment imaging 3D density of overburden, part of a joint study with differential gravity. Muon data were acquired at four locations within a tunnel beneath Los Alamos, New Mexico, and used in a 3D tomographic inversion to recover the spatial variation in the overlying rock–air interface, and compared with a priori knowledge of the topography. Densities obtained exhibit good agreement with preliminary results of the gravity modeling, which will be presented elsewhere, and are compatible with values reported in the literature. The modeled rock–air interface matches that obtained from LIDAR within 4 m, our resolution, over much of the model volume. This experiment demonstrates the power of cosmic ray muons to image shallow geological targets using underground detectors, whose development as borehole devices will be an important new direction of passive geophysical imaging.