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Reaction experiments between tonalitic melt and mantle olivine and their implications for genesis of high-Mg andesites within cratons
Wang MingLiang; Tang HongFeng
Corresponding AuthorTang HongFeng
2013
Source PublicationScience China Earth Sciences
Volume56Issue:11Pages:1918-1925
AbstractHigh-Mg (Mg#> 45) andesites (HMA) within cratons attract great attention from geologists. Their origin remains strongly debated. In order to examine and provide direct evidence for previous assumptions about HMA's genesis inferred from petrological and geochemical investigations, we performed reaction experiments between tonalitic melt and mantle olivine on a six-anvil apparatus at high-temperature of 1250-1400A degrees C and high-pressure of 2.0-5.0 GPa. Our experiments in this work simulated the interaction between the tonalitic melt derived from partial melting of eclogitized lower crust foundering into the Earth's mantle and mantle peridotite. The experimental results show that the reacted melts have very similar variations in chemical compositions to the HMAs within the North China Craton. Therefore, this interaction is probably an important process to generate the HMAs within crations.
KeywordTonalitic Melt Mantle Olivine Melt-mineral Reaction Experiment High-mg Andesite Craton
Subject Area地球深部物质与流体作用地球化学
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/5014
Collection地球内部物质高温高压实验室_地球内部物质高温高压实验室_期刊论文
地球深部物质与流体作用地球化学研究室
Corresponding AuthorTang HongFeng
Recommended Citation
GB/T 7714
Wang MingLiang,Tang HongFeng. Reaction experiments between tonalitic melt and mantle olivine and their implications for genesis of high-Mg andesites within cratons[J]. Science China Earth Sciences,2013,56(11):1918-1925.
APA Wang MingLiang,&Tang HongFeng.(2013).Reaction experiments between tonalitic melt and mantle olivine and their implications for genesis of high-Mg andesites within cratons.Science China Earth Sciences,56(11),1918-1925.
MLA Wang MingLiang,et al."Reaction experiments between tonalitic melt and mantle olivine and their implications for genesis of high-Mg andesites within cratons".Science China Earth Sciences 56.11(2013):1918-1925.
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