Discovery of super-silicic and super-titanic garnets in garnet-pyroxenite in Zhaheba and its geological significance |
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Authors: | HeCai Niu HaiXiang Zhang Qiang Shan XueYuan Yu |
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Institution: | (1) Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, 510640, China |
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Abstract: | Super-silicic garnet which exists stably at more than 5 GPa is a typical ultra-high pressure mineral. The super-silicic garnet
and super-titanic garnet were discovered for the first time in garnet-pyroxenite of early Paleozoic Zhaheba-Aermantai orogenic
belt in north Xinjiang. Our study indicates that these super-silicic garnets as well as super-titanic garnets were formed
at a depth of at least 300 km. Their host rock—garnet-pyroxenite is one kind of ultra-pressure metamorphic rocks which is
related to the ultra-deep subduction of the oceanic crust. Thus, the early Paleozoic Zhaheba-Aermantai orogenic belt is related
to the ultra-deep subduction of the Paleo-Asian oceanic crust.
Supported by the National Natural Science Foundation of China (Grant No. 40673036), and Chinese Academy of Sciences (Grant
Nos. KZCX2-YW-107 and GIGCX-04-03) |
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Keywords: | Zhaheba ophiolite garnet-pyroxenite super-silicic garnet super-titanic garnet ultra-high pressure metamorphism |
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