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An Informative Solution to a Seismological Inverse Problem

Preliminary results are presented that infer that 2 sec should be added to the tabular values for P phases and 4 sec to the tabular values for S phases of seismic travel times. From seismic evidence, the radius of the inner core of the Earth is 1229-1250 km; the radius of the outer core is 3482-3485...

Deskribapen osoa

Gorde:
Xehetasun bibliografikoak
Egile Nagusiak: Gilbert, Freeman, Dziewonski, Adam, Brune, James
Formatua: Artigo
Hizkuntza:Inglês
Argitaratua: 1973
Gaiak:
Sarrera elektronikoa:https://ncbi.nlm.nih.gov/pmc/articles/PMC433508/
https://ncbi.nlm.nih.gov/pubmed/16592083
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