Artigo Revisado por pares

Seismological evidence for roots of mountains

1943; Geological Society of America; Volume: 54; Issue: 4 Linguagem: Inglês

10.1130/gsab-54-473

ISSN

1943-2674

Autores

B. Gutenberg,

Tópico(s)

Geological and Geochemical Analysis

Resumo

Research Article| April 01, 1943 Seismological evidence for roots of mountains BENO GUTENBERG BENO GUTENBERG Search for other works by this author on: GSW Google Scholar Author and Article Information BENO GUTENBERG Publisher: Geological Society of America Received: 22 Jun 1942 First Online: 02 Mar 2017 Online Issn: 1943-2674 Print Issn: 0016-7606 © 1943 Geological Society of America GSA Bulletin (1943) 54 (4): 473–498. https://doi.org/10.1130/GSAB-54-473 Article history Received: 22 Jun 1942 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation BENO GUTENBERG; Seismological evidence for roots of mountains. GSA Bulletin 1943;; 54 (4): 473–498. doi: https://doi.org/10.1130/GSAB-54-473 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Theoretical problems concerned with the calculation of the velocities of seismic waves in the various layers of the earth's crust, and the determination of the thickness of such layers, are discussed. The results are applied to seismograms obtained from artificial explosions, and sources of error in interpretation are investigated. Seismograms registered in different parts of the earth from epicenters less than 1000 km from stations are used to investigate the layering in these regions and the problem of mountain roots. The bearing of the findings on the theory of isostasy is discussed. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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