Age of amphibolites associated with alpine peridotites in the Dinaride ophiolite zone, Yugoslavia
Earth and Planetary Science Letters
By: M. A. Lanphere, R. G. Coleman, S. Karamata, and J. Pamic
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Abstract
Amphibolites associated with alpine peridotites in the Central Ophiolite zone in Yugoslavia have K-Ar ages of 160–170 m.y. These amphibolites and associated peridotites underwent deep-seated metamorphism prior to tectonic emplacement into the sedimentary-volcanic assemblage of the Dinarides. The alpine peridotites and associated local rocks of the ophiolite suite are interpreted as Jurassic oceanic crust and upper mantle.
Suggested Citation
Lanphere, M.A., Coleman, R.G., Karamata, S., Pamic, J., 1975, Age of amphibolites associated with alpine peridotites in the Dinaride ophiolite zone, Yugoslavia: Earth and Planetary Science Letters, v. 26, no. 3, p. 271-276, https://doi.org/10.1016/0012-821X(75)90001-1.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Age of amphibolites associated with alpine peridotites in the Dinaride ophiolite zone, Yugoslavia |
| Series title | Earth and Planetary Science Letters |
| DOI | 10.1016/0012-821X(75)90001-1 |
| Volume | 26 |
| Issue | 3 |
| Year Published | 1975 |
| Language | English |
| Publisher | Elsevier |
| Description | 6 p. |
| First page | 271 |
| Last page | 276 |
| Other Geospatial | Yugoslavia |