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Time of Emergence and Future Projections of Extremes of Malaria Infections in Africa. [PDF]
GeohealthFranzke CLE, Parihar RS.
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, 2019
Preface Acknowledgement 1. Introduction 2. Stress and strain 3. The seismic wave equation 4. Ray theory: travel times 5. Inversion of travel time data 6. Ray theory: amplitude and phase 7. Reflection seismology 8. Surface waves 9.
Peter M. Shearer
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Preface Acknowledgement 1. Introduction 2. Stress and strain 3. The seismic wave equation 4. Ray theory: travel times 5. Inversion of travel time data 6. Ray theory: amplitude and phase 7. Reflection seismology 8. Surface waves 9.
Peter M. Shearer
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Science, 2022
Seismic waves from earthquakes and other sources are used to infer the structure and properties of Earth’s interior. The availability of large-scale seismic datasets and the suitability of deep-learning techniques for seismic data processing have pushed ...
S. Mousavi, G. Beroza
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Seismic waves from earthquakes and other sources are used to infer the structure and properties of Earth’s interior. The availability of large-scale seismic datasets and the suitability of deep-learning techniques for seismic data processing have pushed ...
S. Mousavi, G. Beroza
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Applications of Deep Neural Networks in Exploration Seismology: a technical survey
Geophysics, 2023Exploration seismology uses reflected and refracted seismic waves, emitted from a controlled (active) source into the ground, and recorded by an array of seismic sensors (receivers) to image the subsurface geological structures.
S. Mousavi +3 more
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A diffuse core in Saturn revealed by ring seismology
Nature Astronomy, 2021The best constraints on the internal structures of giant planets have historically originated from measurements of their gravity fields1–3. These data are inherently mostly sensitive to a planet’s outer regions, stymieing efforts to measure the mass and ...
C. Mankovich, J. Fuller
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Surveys in Geophysics, 1993
Since 1969, seismology has been extended beyond the Earth, and seismic sensors have been placed on the surface of other bodies of the solar system. A Lunar seismic network thus operated for the 8 years after 1969, with up to 4 stations, and detected some 1000 Moonquakes per year.
Lognonné, Philippe, Mosser, Benoit
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Since 1969, seismology has been extended beyond the Earth, and seismic sensors have been placed on the surface of other bodies of the solar system. A Lunar seismic network thus operated for the 8 years after 1969, with up to 4 stations, and detected some 1000 Moonquakes per year.
Lognonné, Philippe, Mosser, Benoit
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Science, 1985
Oscillations of the sun make it possible to probe the inside of a star. The frequencies of the oscillations have already provided measures of the sound speed and the rate of rotation throughout much of the solar interior. These quantities are important for understanding the dynamics of the magnetic cycle and have a bearing on testing general relativity
Douglas Gough +2 more
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Oscillations of the sun make it possible to probe the inside of a star. The frequencies of the oscillations have already provided measures of the sound speed and the rate of rotation throughout much of the solar interior. These quantities are important for understanding the dynamics of the magnetic cycle and have a bearing on testing general relativity
Douglas Gough +2 more
openaire +3 more sources