Zobrazeno 1 - 10
of 97
pro vyhledávání: '"George H. Sutton"'
Publikováno v:
The Geophysics of the Pacific Ocean Basin and Its Margin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::05d5d50f6c64b91d57d97e2d783463b9
https://doi.org/10.1029/gm019p0071
https://doi.org/10.1029/gm019p0071
Publikováno v:
The Journal of the Acoustical Society of America. 100:3646-3654
The results of an experiment designed to measure the shear‐wave velocity structure of the shallow‐water sediments at three locations in the East China Sea, in water depths ranging from 40 m to 150 m, are reported. Both vertically polarized and ho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8034f93067aa75cdddfca9c1c06de7c5
https://doi.org/10.1121/1.417227
https://doi.org/10.1121/1.417227
Autor:
George H. Sutton, Noël Barstow
Publikováno v:
Geophysical Research Letters. 23:499-502
In this paper we describe microseisms and swell produced by a supertyphoon in the western Pacific, near the Philippine Islands, recorded from an ocean-bottom seismic ‘station’ (OBSS) located about 200 km west of San Francisco, California at a dep
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9ad02be31286e1bf4f5319d3587b38f2
https://doi.org/10.1029/96gl00419
https://doi.org/10.1029/96gl00419
Autor:
George H. Sutton, F.K. Duennebier
Publikováno v:
Marine Geophysical Researches. 17:535-555
The often poor quality of ocean bottom seismic data, particularly that observed on horizontal seismometers, is shown to be the result of instruments responding to motions in ways not intended. Instruments designed to obtain the particle motion of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e7e89b272d3e3558ea4353896cd35e4d
https://doi.org/10.1007/bf01204343
https://doi.org/10.1007/bf01204343
Publikováno v:
The Journal of the Acoustical Society of America. 93:2639-2648
One year of ambient ocean noise data, 0.4 to 30 Hz, from the Wake Island hydrophone array in the northwestern Pacific are compared to surface wind speeds, 0–14 m/s (0–28 kn). Between 0.4 and 6 Hz, noise levels increase with wind speed at rates of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::71937f8bc27ddb96129e800c93a43806
https://doi.org/10.1121/1.405838
https://doi.org/10.1121/1.405838
Autor:
Patricia A. Berge, Gerard J. Fryer, John I. Ewing, Jerry A. Carter, George H. Sutton, Noël Barstow, Subhashis Mallick
Publikováno v:
Geophysical Journal International. 104:241-254
SUMMARY The interleaving of parallel isotropic lamellae of contrasting mineralogical composition makes almost all marine sediments anisotropic, the form of anisotropy being transverse isotropy with a vertical axis of symmetry. Conventional marine sei
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a32a6436edd0dc0db5d75e8ea9aa2847
https://doi.org/10.1111/j.1365-246x.1991.tb02509.x
https://doi.org/10.1111/j.1365-246x.1991.tb02509.x
Autor:
George H. Sutton, Noel Barstow
Publikováno v:
The Journal of the Acoustical Society of America. 87:2005-2012
Observed spatial and temporal characteristics of ultralow‐frequency (ULF) ocean‐bottom seismo‐acoustic ambient noise are required in order to construct realistic quantitative predictive models of the phenomena involved. Few such data exist or h
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c609015ab3a20e598da5c4ed2693dd6c
https://doi.org/10.1121/1.399328
https://doi.org/10.1121/1.399328
Autor:
Patrick J. Leahy, George H. Sutton, Paul W. Pomeroy, Noel Barstow, Eric P. Chael, Jerry A. Carter
Publikováno v:
Geophysical Research Letters. 17:681-684
Seismograms of noise recorded simultaneously at the surface and at two subsurface stations (335m and 945m below surface level) show that high frequency (1-100 Hz) background noise is reduced at the subsurface stations. Seismometers at all three stati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b7c2d52284b3905940ca9a197c6ed140
https://doi.org/10.1029/gl017i006p00681
https://doi.org/10.1029/gl017i006p00681
Autor:
F.K. Duennebier, George H. Sutton
Publikováno v:
Geochemistry, Geophysics, Geosystems. 8
[1] Theory, testing, and use of ocean bottom seismic sensors show that the fidelity of data, particularly measurements of horizontal motion, can be severely distorted and noisy because of mechanical interactions between the sensor package, the ocean
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cc1282ea7a036305ded1b8388421d4f9
https://doi.org/10.1029/2006gc001428
https://doi.org/10.1029/2006gc001428
Autor:
Jerry A. Carter, Noel Barstow, George H. Sutton, Patricia A. Berge, Subhashis Mallick, John I. Ewing, Gerard J. Fryer
Publikováno v:
Shear Waves in Marine Sediments ISBN: 9789401055819
In 1986, an on-bottom shear wave source and a multi-component on-bottom receiver with a hydrophone were used by Woods Hole Oceanographic Institution and Rondout Associates, Inc. to record a short (< 200m) refraction profile near the United States Geo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::241dc1fe664798a6b1fddd134ad6c793
https://doi.org/10.1007/978-94-011-3568-9_23
https://doi.org/10.1007/978-94-011-3568-9_23