In general, microseisms are a nuisance. It is now quite widely agreed that microseisms are channel waves, similar in nature to the Lg and Rg waves. It is not at all unusual to observe microseisms which have traveled over distances of continental proportions. In order to determine the direction from which the microseisms come and to investigate in more detail the characteristics of microseismic disturbances, we established a tri-partite system on Mount Palomar
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/108317/1/eost23200228.pd
The paper contains the results of a survey of microseisms throughout the world during January, 1930,...
Microseisms are more or less regular elastic surface waves recorded continuously by sensitive seismo...
Ever since the beginning of instrumental seismology the problem of microseisms has been a subject of...
Our most sensitive seismographs are never at rest. They show that there are always small movements ...
This paper reviews the various problems of research on microseisms, and also the method of obtaining...
Thesis. (Sc.D.) Massachusetts Institute of Technology. Dept. of Geology and Geophysics, 1954.Vita.Bi...
Primary microseisms are background seismic oscillations recorded everywhere on Earth with typical fr...
Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Geology and Geophysics, 1961.Includes...
For some 40 years it has been known as a result of seismograph observations that the ground is never...
In the previous paper (Okano 1961) it was shown that microseismic waves are generated by the swells ...
Some aspects of Rayleigh wave propagation on the North American continent have been deduced from the...
This paper discusses the use of microseism measurement as a tool to predict local site amplification...
In the absence of earthquakes, oceanic microseisms are the strongest signals recorded by seismic sta...
Analysis of spatially coherent seafloor motion is conducted using data from two ocean bottom seismom...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/108317/1/eost23200228.pd
The paper contains the results of a survey of microseisms throughout the world during January, 1930,...
Microseisms are more or less regular elastic surface waves recorded continuously by sensitive seismo...
Ever since the beginning of instrumental seismology the problem of microseisms has been a subject of...
Our most sensitive seismographs are never at rest. They show that there are always small movements ...
This paper reviews the various problems of research on microseisms, and also the method of obtaining...
Thesis. (Sc.D.) Massachusetts Institute of Technology. Dept. of Geology and Geophysics, 1954.Vita.Bi...
Primary microseisms are background seismic oscillations recorded everywhere on Earth with typical fr...
Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Geology and Geophysics, 1961.Includes...
For some 40 years it has been known as a result of seismograph observations that the ground is never...
In the previous paper (Okano 1961) it was shown that microseismic waves are generated by the swells ...
Some aspects of Rayleigh wave propagation on the North American continent have been deduced from the...
This paper discusses the use of microseism measurement as a tool to predict local site amplification...
In the absence of earthquakes, oceanic microseisms are the strongest signals recorded by seismic sta...
Analysis of spatially coherent seafloor motion is conducted using data from two ocean bottom seismom...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/108317/1/eost23200228.pd
The paper contains the results of a survey of microseisms throughout the world during January, 1930,...
Microseisms are more or less regular elastic surface waves recorded continuously by sensitive seismo...