Mineralogical Features and Properties of Serpentine as Indicator of the Deep Earth Subduction Processes
The article presents the results of study of composition, structure and properties of three genetic types of serpentinite, developed by chromite-bearing ultrabasic rocks, by metamorphic zones of carbonate rocks and within the zone of weathering of ultrabasic rocks. The samples were selected from dep...
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| Veröffentlicht in: | 地球科学与工程：英文版 2012, Vol.2 (12), p.729-743 |
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| container_title | 地球科学与工程：英文版 |
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| creator | Tatiana V. Posukhova Leily L Elene B. Cherepetskaya Ivan E. Sas |
| description | The article presents the results of study of composition, structure and properties of three genetic types of serpentinite, developed by chromite-bearing ultrabasic rocks, by metamorphic zones of carbonate rocks and within the zone of weathering of ultrabasic rocks. The samples were selected from deposits, located along the Main Ural Fault-the Paleozoic subduction zone （named GUR）. Peculiarities of microstructure, chemical composition and properties of serpentinites formed in different geological conditions were investigated and their comparative study was held. They were devided three groups of serpentinites with oriented and non-oriented structure which formed by different protholites： mantle, lithosphere and crust. |
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| ispartof | 地球科学与工程：英文版, 2012, Vol.2 (12), p.729-743 |
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| language | eng |
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| source | EZB-FREE-00999 freely available EZB journals |
| subjects | 俯冲带 地球深部 属性 微观结构 特征和 矿物学 蛇纹石 超基性岩 |
| title | Mineralogical Features and Properties of Serpentine as Indicator of the Deep Earth Subduction Processes |
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