Zobrazeno 1 - 10
of 81
pro vyhledávání: '"B. Knapmeyer-Endrun"'
Autor:
C. Finger, M. P. Roth, M. Dietl, A. Gotowik, N. Engels, R. M. Harrington, B. Knapmeyer-Endrun, K. Reicherter, T. Oswald, T. Reinsch, E. H. Saenger
Publikováno v:
Earth System Science Data, Vol 15, Pp 2655-2666 (2023)
Passive seismic analyses are a key technology for the exploration and monitoring of subsurface reservoirs. Searching for alternative resources in the framework of the energy transition is creating a surge for identifying as many potential sites as po
Externí odkaz:
https://doaj.org/article/1b3b2c499cba40c1b6cbf4bd12f50be3
Autor:
D. Kim, C. Duran, D. Giardini, A.‐C. Plesa, S. C. Stähler, C. Boehm, V. Lekić, S. M. McLennan, S. Ceylan, J. F. Clinton, P. Davis, A. Khan, B. Knapmeyer‐Endrun, M. P. Panning, M. Wieczorek, P. Lognonné, W. B. Banerdt
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 12, Pp n/a-n/a (2023)
Abstract We report observations of Rayleigh waves that orbit around Mars up to three times following the S1222a marsquake. Averaging these signals, we find the largest amplitude signals at 30 and 85 s central period, propagating with distinctly diffe
Externí odkaz:
https://doaj.org/article/03f479783e1e41d3ac4b745a8b2691e7
Autor:
S. Menina, L. Margerin, T. Kawamura, G. Heller, M. Drilleau, Z. Xu, M. Calvet, R. F. Garcia, B. Knapmeyer‐Endrun, S. Carrasco, K. Onodera, P. Lognonné, A. Stott, W. B. Banerdt
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 7, Pp n/a-n/a (2023)
Abstract We have modeled the high‐frequency seismogram envelopes of the large event S1222a and four recently identified near impacts recorded by the InSight mission by introducing a stratification of velocity and attenuation into a multiple‐scatt
Externí odkaz:
https://doaj.org/article/9a80c3ffb5f2442c884c9e9453d7ade4
Autor:
J. Shi, M. Plasman, B. Knapmeyer‐Endrun, Z. Xu, T. Kawamura, P. Lognonné, S. M. McLennan, G. Sainton, W. B. Banerdt, M. P. Panning, T. Wang
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 5, Pp n/a-n/a (2023)
Abstract The shallow crustal structure of Mars records the evolutionary history of the planet, which is crucial for understanding the early Martian geological environment. Until now, seismic constraints on the Martian crust have come primarily from t
Externí odkaz:
https://doaj.org/article/46b743039ddd4861a1e64494d590e977
Autor:
M. P. Panning, W. B. Banerdt, C. Beghein, S. Carrasco, S. Ceylan, J. F. Clinton, P. Davis, M. Drilleau, D. Giardini, A. Khan, D. Kim, B. Knapmeyer‐Endrun, J. Li, P. Lognonné, S. C. Stähler, G. Zenhäusern
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 1, Pp n/a-n/a (2023)
Abstract Prior to the 2018 landing of the InSight mission, the InSight science team proposed locating Marsquakes using multiple orbit surface waves, independent of seismic velocity models, for events larger than MW4.6. The S1222a MW4.7 of 4 May 2022
Externí odkaz:
https://doaj.org/article/e58f3611e7924e8797e4bb5dadaed871
Autor:
M. Hobiger, M. Hallo, C. Schmelzbach, S. C. Stähler, D. Fäh, D. Giardini, M. Golombek, J. Clinton, N. Dahmen, G. Zenhäusern, B. Knapmeyer-Endrun, S. Carrasco, C. Charalambous, K. Hurst, S. Kedar, W. B. Banerdt
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-13 (2021)
We invert Rayleigh wave ellipticity curves extracted from ambient seismic vibrations at the InSight landing site to resolve, for the first time on Mars, the shallow subsurface to around 200 m depth. While our seismic velocity model is largely consist
Externí odkaz:
https://doaj.org/article/981e593d21b04915984d2f1606bda1f5
Publikováno v:
Results in Physics, Vol 7, Iss , Pp 4457-4458 (2017)
Using a novel pattern recognition algorithm, up to 50,000 new seismic events have been detected on the Moon over an 8-month period from newly rediscovered Apollo 17 seismic data. These events occur periodically, with a sharp double-peak at sunrise an
Externí odkaz:
https://doaj.org/article/ac58e497c58c4f09a2521e8d92da540a
Autor:
D. Kim, W. B. Banerdt, S. Ceylan, D. Giardini, V. Lekić, P. Lognonné, C. Beghein, É. Beucler, S. Carrasco, C. Charalambous, J. Clinton, M. Drilleau, C. Durán, M. Golombek, R. Joshi, A. Khan, B. Knapmeyer-Endrun, J. Li, R. Maguire, W. T. Pike, H. Samuel, M. Schimmel, N. C. Schmerr, S. C. Stähler, E. Stutzmann, M. Wieczorek, Z. Xu, A. Batov, E. Bozdag, N. Dahmen, P. Davis, T. Gudkova, A. Horleston, Q. Huang, T. Kawamura, S. D. King, S. M. McLennan, F. Nimmo, M. Plasman, A. C. Plesa, I. E. Stepanova, E. Weidner, G. Zenhäusern, I. J. Daubar, B. Fernando, R. F. Garcia, L. V. Posiolova, M. P. Panning
Publikováno v:
Science, 378 (6618)
Kim, D, Banerdt, W B, Ceylan, S, Horleston, A C, Giardini, D, et, A & Lekić, V 2022, ' Surface Waves and Crustal Structure on Mars ', Science, vol. 378, no. 6618, pp. 417-421 . https://doi.org/10.1126/science.abq7157
Kim, D, Banerdt, W B, Ceylan, S, Horleston, A C, Giardini, D, et, A & Lekić, V 2022, ' Surface Waves and Crustal Structure on Mars ', Science, vol. 378, no. 6618, pp. 417-421 . https://doi.org/10.1126/science.abq7157
We detected surface waves from two meteorite impacts on Mars. By measuring group velocity dispersion along the impact-lander path, we obtained a direct constraint on crustal structure away from the InSight lander. The crust north of the equatorial di
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Akademický článek
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