Diamonds in an upper mantle peridotite nodule from kimberlite in southern wyoming
Science
By: M. E. McCallum and D.H. Eggler
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Abstract
Diamonds in a serpentinized garnet peridotite nodule from a diatreme in southern Wyoming are the first known occurrence in an upper mantle peridotite xenolith from a kimberlite intrusion in North America as well as the second authenticated occurrence of diamonds from kimberlite pipes in North America. The nodule is believed to have come from a section of depleted (partially melted) Iherzolite at a depth of 130 to 180 kilometers.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Diamonds in an upper mantle peridotite nodule from kimberlite in southern wyoming |
| Series title | Science |
| Volume | 192 |
| Issue | 4236 |
| Year Published | 1976 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Science |
| First page | 253 |
| Last page | 256 |
| Google Analytic Metrics | Metrics page |