Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Herbert R. Shaw"'
Publikováno v:
The Geophysics of the Pacific Ocean Basin and Its Margin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b90da1051e9ce96b45eabcffabf4bac3
https://doi.org/10.1029/gm019p0375
https://doi.org/10.1029/gm019p0375
Autor:
Bernard Chouet, Herbert R. Shaw
Publikováno v:
Journal of Geophysical Research. 96:10191
A hierarchical model of magma transport in Hawaii is developed from the seismic records of deep (30–60 km) and intermediate-depth (5–15 km) harmonic tremor between January 1, 1962, and December 31, 1983. We find two kinds of spatial distributions
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6f1b78924ea15a13ee4db2ce470c2bd6
https://doi.org/10.1029/91jb00771
https://doi.org/10.1029/91jb00771
Autor:
Herbert R. Shaw, Bernard Chouet
Publikováno v:
Journal of Geophysical Research. 96:10177
We study the fractal properties of shallow volcanic tremor and gas piston events associated with magma degassing at Kilauea Volcano, Hawaii, using data from two dense short-baseline arrays of seismographs deployed near the active crater of Puu Oo on
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e8aa3f5826c6956f57db1c3ed59f39a5
https://doi.org/10.1029/91jb00772
https://doi.org/10.1029/91jb00772
Autor:
Herbert R. Shaw, Bernard Chouet
Publikováno v:
Geophysical Research Letters. 16:195-198
Fractal singularity analysis (FSA) is used to study a 22-year record of deep seismic tremor (30–60 km depth) for regions below Kilauea Volcano on the assumption that magma transport and fracture can be treated as a system of coupled nonlinear oscil
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba53d60c018ce51a67625a0fbae7a5d3
https://doi.org/10.1029/gl016i002p00195
https://doi.org/10.1029/gl016i002p00195
Stress fields in central portions of the Pacific Plate: Delineated in time by linear volcanic chains
Autor:
Everett D. Jackson, Herbert R. Shaw
Publikováno v:
Journal of Geophysical Research. 80:1861-1874
Many linear island chains in the Pacific appear to consist of individual volcanic shields that lie on relatively short, curved loci sometimes of sigmoidal form. These loci, in turn, lie at an angle to the directions of propagation of the chains. Thos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e01697ea0c052c3a6283f4d329abc208
https://doi.org/10.1029/jb080i014p01861
https://doi.org/10.1029/jb080i014p01861
Publikováno v:
Earth and Planetary Science Letters. 26:145-155
A new method has been discovered for calculating ages of the main shield building stages of volcanoes along the Hawaiian chain from Kilauea to the Hawaiian-Emperor bend. The method is based on a graphical technique for hypothetical subtraction of dis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dd50da29d9df770fb7e8602497b5d23e
https://doi.org/10.1016/0012-821x(75)90082-5
https://doi.org/10.1016/0012-821x(75)90082-5
Autor:
Herbert R. Shaw
Publikováno v:
Journal of Petrology. 10:510-535
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b68a9ec5bffbfdc0142fe79c88a55adc
https://doi.org/10.1093/petrology/10.3.510
https://doi.org/10.1093/petrology/10.3.510
Autor:
Herbert R. Shaw
Publikováno v:
The Journal of Geology. 72:601-617
Simple statistical mechanical models are applied to calculate thermodynamic properties of liquid silicate-$H_{2}O$ mixtures. From these models relative activities for binary silicate-$H_{2}O$ mixtures have been derived both for structural units of eq
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e081d454a41da89107383a5f517964cb
https://doi.org/10.1086/627016
https://doi.org/10.1086/627016
Autor:
Herbert R. Shaw
Publikováno v:
Science. 168:1084-1087
The power of a heat engine ignited by tidal energy can account for geologically reasonable rates of average magma production and sea floor spreading. These rates control similarity of heat flux over continents and oceans because of an inverse relatio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d3efd459899588fd1309d377448ea132
https://doi.org/10.1126/science.168.3935.1084
https://doi.org/10.1126/science.168.3935.1084