Danburite in evaporites of the Paradox basin, Utah.
Journal of Sedimentary Petrology
By: O.B. Raup and B.M. Madsen
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Abstract
Danburite (CaB2Si2O8) has been found as nodules in Pennsylvanian age marine evaporites. The occurrence of danburite and its relation to the host rock in the Paradox basin evaporites indicates that it most likely formed by diagenetic reaction of boron-rich, high-salinity brines with constituents in the anhydrite host rock.-from Authors
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Danburite in evaporites of the Paradox basin, Utah. |
| Series title | Journal of Sedimentary Petrology |
| Volume | 56 |
| Issue | 2 |
| Year Published | 1986 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Journal of Sedimentary Petrology |
| First page | 248 |
| Last page | 251 |
| Google Analytic Metrics | Metrics page |