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- W2123464618 abstract "The SarÝkaraman Ophiolite is one of the least dismembered ophiolitic units of the allochthonous Central Anatolian Ophiolites, which retains its recognizable pseudostratigraphy. The SarÝkaraman Ophiolite is represented in its lowermost part by isotropic gabbros. Within the isotropic gabbro sequence, clinopyroxenes are observed as small, colorless relicts with a cloudy appearance. In most of the samples, they are completely replaced by a successive generation of green to brown amphiboles. Clinopyroxenes display diopsitic to augitic compositions within the range of En45Fs5Wo49 to En50Fs9Wo41. They are Ca-rich and Na- poor (Na2O<0.55) and characterized by high-Mg (Mg#= 81.4-91.19) and low-Ti (<0.68 wt %). The occurrence of a high-Mg and low-Ti magma constrain the formation of the SarÝkaraman ophiolitic gabbro in a supra-subduction zone environment. The clinopyroxenes of the Middle Turonian-Lower Campanian SarÝkaraman Ophiolite have similar chemical com- positions to those of the other supra-subduction zone-type Eastern Mediterranean ophiolites (e.g., Troodos, Varinous, Pindos and Oman ophiolites) that show island-arc affinity." @default.
- W2123464618 created "2016-06-24" @default.
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- W2123464618 date "1999-02-01" @default.
- W2123464618 modified "2023-09-24" @default.
- W2123464618 title "Clinopyroxene Compositions of the Isotropic Gabbros From the Sarıkaraman Ophiolite: New Evidence on Supra-Subduction Zone Type Magma Genesis in Central Anatolia" @default.
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