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- W2023340791 abstract "This paper summaries tectonic settings and mineral parageneses of several recognized ultrahigh-pressure (UHP) terranes other than the well-studied Kokchetav Massif of northern Kazakhstan, the Western Gneiss Region of Norway, the Dora-Maira massif of the Western Alps, and the Dabie-Sulu terrane of east-central China. Diamond-bearing terranes include the Beni Bousera/Ronda peridotite massif, the Erzgebirge Crystalline Complex, mantle peridotite from a Tibetan ophiolite, and possibly the Maksyutov Complex. Coesite-bearing UHP terranes are the Zermatt-Saas area, Western Alps; the Mali eclogites from West Africa; the Makabal complex of western Tien Shan; the Bohemian massif; and the newly reported Central Indonesia terrane and Himalayan eclogites from the upper Kaghan Valley of Pakistan. Except for the diamond-bearing Tibetan ophiolite, most UHP terranes share similar petrotectonic assemblages and lie within major continental collision belts in Eurasia and Africa. Using new approaches (including new geobarometers) and technologies, additional UHP terranes are expected to be recognized in other Phanenorozic orogenic sutures." @default.
- W2023340791 created "2016-06-24" @default.
- W2023340791 creator A5071599901 @default.
- W2023340791 date "1999-07-01" @default.
- W2023340791 modified "2023-10-17" @default.
- W2023340791 title "Petrotectonic Summary of Less Intensively Studied UHP Regions" @default.
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- W2023340791 doi "https://doi.org/10.1080/00206819909465158" @default.
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