Si- and alkali-rich melt inclusions in minerals of mantle peridotites from eastern China: Implication for lithospheric evolution |
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摘 要: | CO2 fluid inclusions in mantle minerals are an im-portant source for us to get the information of mantle fluids. Fluid inclusions are mainly composed of CO2, with minor CO, H2O, CH4, N2, H2S, SO2, F, etc., which were demonstrated by lots of Raman spec-trometer analyses in recent years. In contrast, there are very few researches on CO2-bearing melt inclusions since it is more difficult to do so. The available studies have found that the primary CO2-bearing melt inclu-sions are basaltic …
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收稿时间: | 16 March 2005 |
修稿时间: | 23 June 2005 |
Si-and alkali-rich melt inclusions in minerals of mantle peridotites from eastern China: Implication for lithospheric evolution |
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Authors: | FAN Qicheng SUI Jianli XU Ping LI Ni SUN Qian WANG Tuanhua |
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Institution: | 1. Institute of Geology, China Seismological Bureau, Beijing 100029, China 2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China |
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Abstract: | Minerals of spinel-and garnet-facies mantle xenoliths entrained in Cenozoic basalts from eastern China (North China, Northeastern
China and Southeastern China coastal area) contains lots of melt inclusions. Studies on these melt inclusions show that the
glass inclusions are rich in SiO2 (60%-68%) and alkalis (K2O+Na2O=5%-11%, especially for K2O) as well as volatiles such as H2O and CO2 (2%-7%), which belong to dacites and andesites of the high-K calcic alkali series rocks with few shoshonites. High Al and
Ca diopside in melt inclusion is the product of melt crystallization at high temperature and pressure, rather than the product
of devitrification. Results show that these K-rich (in general K2O>3%) intermediate-acidic silicate melt inclusions have characteristics of continent without a genetical link to host basalts
and their phenocrystic minerals. Thus, these trapped melt inclusions represent melts of Mesozoic lithospheric mantle-crust
interaction and imply that the continental lithospheric mantle beneath eastern China had undergone fragmentation and recreation
processes during the Mesozoic and Cenozoic periods. This result undoubtly provides important implication for the evolution
of sub-continental lithosphere beneath eastern China. We propose that these Si-and alkalis-rich melts should be responsible
for the mantle chemical heterogeneity underneath eastern China. |
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Keywords: | Si- and alkali-rich melt inclusion mantle peridotite lithospheric evolution eastern China |
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