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Diatremes with kimberlitic affinities in North-Central Montana

January 1, 1968

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 Year 1968
Title Diatremes with kimberlitic affinities in North-Central Montana
Authors B. C. Hearn
Publication Type Article
Publication Subtype Journal Article
Series Title Science
Index ID 70011641
Record Source USGS Publications Warehouse