Fifth Presentation of the James B. Macelwane Award, April 20, 1966
Don Anderson was born in Frederick, Maryland, thirty-three years ago. He took his Bachelor's degree at Rennselaer Polytechnic Institute in 1955. Between 1955 and 1958 he worked for Chevron Oil Company, served in the Air Force, and conducted research for the Arctic Institute of North America. He...
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1966
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ftcaltechauth:oai:authors.library.caltech.edu:dbtk0-9de93 2024-06-23T07:49:00+00:00 Fifth Presentation of the James B. Macelwane Award, April 20, 1966 Droessler, G. Slichter, Louis B. 1966-06 https://doi.org/10.1029/TR047i002p00361 unknown American Geophysical Union https://doi.org/10.1029/TR047i002p00361 oai:authors.library.caltech.edu:dbtk0-9de93 eprintid:62874 resolverid:CaltechAUTHORS:20151214-114154226 info:eu-repo/semantics/openAccess Other Eos, 47(2), 361-362, (1966-06) info:eu-repo/semantics/article 1966 ftcaltechauth https://doi.org/10.1029/TR047i002p00361 2024-06-12T01:49:16Z Don Anderson was born in Frederick, Maryland, thirty-three years ago. He took his Bachelor's degree at Rennselaer Polytechnic Institute in 1955. Between 1955 and 1958 he worked for Chevron Oil Company, served in the Air Force, and conducted research for the Arctic Institute of North America. He received his Ph.D. from Caltech in 1962, where he currently serves as Associate Professor of Geophysics. Don L. Anderson has utilized the range of modern observations concerning seismic body and surface waves, the free vibrations, and the loss characteristics of all these to re-evaluate and to revise interpretations of the elastic and anelastic structure of the Earth. He has analyzed recent observations of large artificial explosions to elucidate the complex events in the epicentral range 10°–40°, where he finds that a succession of triple-valued travel-time curves appears to occur. These curves are interpreted in terms of two regions of rapid increase in both velocity and density, one at the bottom of the Gutenberg low-speed zone at depth 300 km, the other at depth 600 km. These interpretations are consistent with the results from free-mode observations. The two levels of rapid changes may represent zones of phase change. In the lower mantle, the density increases very slowly relative to the rates in the earlier Earth models. © 1966 American Geophysical Union. Published - DLAagu66.pdf Article in Journal/Newspaper Arctic Institute of North America Arctic The Arctic Institute Caltech Authors (California Institute of Technology) Arctic Macelwane ENVELOPE(-89.500,-89.500,-81.900,-81.900) Eos, Transactions American Geophysical Union 47 2 361 362 |
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Open Polar |
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Caltech Authors (California Institute of Technology) |
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ftcaltechauth |
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unknown |
description |
Don Anderson was born in Frederick, Maryland, thirty-three years ago. He took his Bachelor's degree at Rennselaer Polytechnic Institute in 1955. Between 1955 and 1958 he worked for Chevron Oil Company, served in the Air Force, and conducted research for the Arctic Institute of North America. He received his Ph.D. from Caltech in 1962, where he currently serves as Associate Professor of Geophysics. Don L. Anderson has utilized the range of modern observations concerning seismic body and surface waves, the free vibrations, and the loss characteristics of all these to re-evaluate and to revise interpretations of the elastic and anelastic structure of the Earth. He has analyzed recent observations of large artificial explosions to elucidate the complex events in the epicentral range 10°–40°, where he finds that a succession of triple-valued travel-time curves appears to occur. These curves are interpreted in terms of two regions of rapid increase in both velocity and density, one at the bottom of the Gutenberg low-speed zone at depth 300 km, the other at depth 600 km. These interpretations are consistent with the results from free-mode observations. The two levels of rapid changes may represent zones of phase change. In the lower mantle, the density increases very slowly relative to the rates in the earlier Earth models. © 1966 American Geophysical Union. Published - DLAagu66.pdf |
format |
Article in Journal/Newspaper |
author |
Droessler, G. Slichter, Louis B. |
spellingShingle |
Droessler, G. Slichter, Louis B. Fifth Presentation of the James B. Macelwane Award, April 20, 1966 |
author_facet |
Droessler, G. Slichter, Louis B. |
author_sort |
Droessler, G. |
title |
Fifth Presentation of the James B. Macelwane Award, April 20, 1966 |
title_short |
Fifth Presentation of the James B. Macelwane Award, April 20, 1966 |
title_full |
Fifth Presentation of the James B. Macelwane Award, April 20, 1966 |
title_fullStr |
Fifth Presentation of the James B. Macelwane Award, April 20, 1966 |
title_full_unstemmed |
Fifth Presentation of the James B. Macelwane Award, April 20, 1966 |
title_sort |
fifth presentation of the james b. macelwane award, april 20, 1966 |
publisher |
American Geophysical Union |
publishDate |
1966 |
url |
https://doi.org/10.1029/TR047i002p00361 |
long_lat |
ENVELOPE(-89.500,-89.500,-81.900,-81.900) |
geographic |
Arctic Macelwane |
geographic_facet |
Arctic Macelwane |
genre |
Arctic Institute of North America Arctic The Arctic Institute |
genre_facet |
Arctic Institute of North America Arctic The Arctic Institute |
op_source |
Eos, 47(2), 361-362, (1966-06) |
op_relation |
https://doi.org/10.1029/TR047i002p00361 oai:authors.library.caltech.edu:dbtk0-9de93 eprintid:62874 resolverid:CaltechAUTHORS:20151214-114154226 |
op_rights |
info:eu-repo/semantics/openAccess Other |
op_doi |
https://doi.org/10.1029/TR047i002p00361 |
container_title |
Eos, Transactions American Geophysical Union |
container_volume |
47 |
container_issue |
2 |
container_start_page |
361 |
op_container_end_page |
362 |
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1802639289038667776 |