May 1, 1989

The Nature of Deep-Focus Earthquakes

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Resumen

Carbonatites are igneous rocks formed in the crust by fractional crystallization of carbonate-rich parental melts that are mostly mantle derived. They dominantly consist of carbonate minerals such as calcite, dolomite, and ankerite, as well as minor ...Read More

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Cite This Study

Cliff Frohlich (Mon,) studied this question.

synapsesocial.com/papers/6a157cbe5347fbb1739fdb18 https://doi.org/https://doi.org/10.1146/annurev.ea.17.050189.001303

Also Consider

Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context:

1The Japanese earthquake of March 29, 1928, and the problem of depth of focus11932 · 23 citations
2Observations of body wave multipathing from broadband seismograms: Evidence for lower mantle slab penetration beneath the Sea of Okhotsk1986 · 83 citations
3The energy release in great earthquakes1977 · 2,466 citations
4Source wave forms of three earthquakes1963 · 57 citations
5Depth and geographical distribution of deep-focus earthquakes1938 · 46 citations

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