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.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Diatremes with kimberlitic affinities in North-Central Montana |
| Series title | Science |
| Volume | 159 |
| Issue | 3815 |
| Year Published | 1968 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Science |
| First page | 622 |
| Last page | 625 |
| Google Analytic Metrics | Metrics page |