Show simple item record

dc.contributor.advisorStephen M. Simpson, Jr.en_US
dc.contributor.authorGreenfield, Royen_US
dc.contributor.otherMassachusetts Institute of Technology. Dept. of Geology and Geophysics.en_US
dc.date.accessioned2010-04-07T13:37:56Z
dc.date.available2010-04-07T13:37:56Z
dc.date.issued1962en_US
dc.identifier.urihttp://hdl.handle.net/1721.1/53533
dc.descriptionThesis (M.S.)--Massachusetts Institute of Technology, Dept. of Geology and Geophysics, 1962.en_US
dc.description"June 1962."en_US
dc.descriptionIncludes bibliographical references (leaf 73).en_US
dc.description.abstractThe response to a harmonic point source in a liquid layer overlying a liquid half space is computed as a function of frequency. Included are the contributions form all normal modes that occur, and the branch-line integral representing the refraction arrival. The value of the refraction arrival is given in terms of the complex error function. The effect of different velocity and density contrasts are considered, and the effect of source depth and the distance to the receiver are investigated. The results giving the behavior of the magnitude of the branch line show that it is much larger at the mode cutoffs than at other values of frequency. The total amplitude of the response shows a regular oscillation in the frequency range in which two modes are present, and somewhat irregular high and low values over the range in which three modes are present. This behavior reflects the difference in amplitude at frequencies for which modes reinforce or interfere with each other.en_US
dc.description.statementofresponsibilityby Roy J. Greenfield.en_US
dc.format.extent73 leavesen_US
dc.language.isoengen_US
dc.publisherMassachusetts Institute of Technologyen_US
dc.rightsM.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.en_US
dc.rights.urihttp://dspace.mit.edu/handle/1721.1/7582en_US
dc.subjectGeology and Geophysics.en_US
dc.titleThe response of a point source in a liquid layer overlying a liquid half spaceen_US
dc.typeThesisen_US
dc.description.degreeM.S.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Geology and Geophysicsen_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
dc.identifier.oclc33195329en_US


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record