Diatremes with kimberlitic affinities in north-central Montana
Science
By: B. C. Hearn Jr.
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Abstract
Diatremes in the Missouri River Breaks demonstrate systematic subsidence-ring structure, contain inclusions derived from far above and far below, and have been produced by gas-rich eruptions of alkalic ultramafic magmas. Similar magmas have produced diatremes in many localities in the world and are known to be closely associated with and probably parental to kimberlites.
Suggested Citation
Hearn, B.C., 1968, Diatremes with kimberlitic affinities in north-central Montana: Science, v. 159, no. 3815, p. 622-625, https://doi.org/10.1126/science.159.3815.622.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Diatremes with kimberlitic affinities in north-central Montana |
| Series title | Science |
| DOI | 10.1126/science.159.3815.622 |
| Volume | 159 |
| Issue | 3815 |
| Year Published | 1968 |
| Language | English |
| Publisher | American Association for the Advancement of Science |
| Description | 4 p. |
| First page | 622 |
| Last page | 625 |
| Country | United States |
| State | Montana |
| Other Geospatial | Missouri River Breaks, north-central Montana |