Anomalous delays of teleseismic P waves in Yellowstone National Park
Nature
By: H. M. Iyer
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Abstract
TELESEISMIC P waves recorded by a short-period seismic network, comprising 12 stations, in Yellowstone National Park, show anomalous delays of 1–2 s in their travel times in the central region of the park relative to the surrounding area. To explain this phenomenon, I propose that a substantial body of low velocity material is present beneath the park, with horizontal dimensions of several tens of kilometres; it may be the magma chamber associated with the volcanism of Yellowstone (ref. 1, and G. P. Eaton et al., unpublished).
Suggested Citation
Iyer, H.M., 1975, Anomalous delays of teleseismic P waves in Yellowstone National Park: Nature, v. 253, no. 5491, p. 425-427, https://doi.org/10.1038/253425a0.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Anomalous delays of teleseismic P waves in Yellowstone National Park |
| Series title | Nature |
| DOI | 10.1038/253425a0 |
| Volume | 253 |
| Issue | 5491 |
| Year Published | 1975 |
| Language | English |
| Publisher | Nature |
| Description | 3 p. |
| First page | 425 |
| Last page | 427 |
| Country | United States |
| State | Wyoming |
| Other Geospatial | Yellowstone National Park |