Two A—type Syenite—Granite Belts in Anhui |
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摘 要: |
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关 键 词: | A型花岗岩 安徽 稀土元素 黑花岗石 成因 |
Two A-type syenite-granite belts in Anhui |
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Authors: | Xing Fengming Xu Xiang |
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Institution: | (1) Anhui Institute of Geological Sciences, 230001 Hefei |
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Abstract: | There exist two parallel A-type syenite-granite belts on both banks of the Yangtze River in Anhui Province: one is the Dalongshan-Chengshan-Huangmeijian
belt on the north bank and the other is the Huayuangong-Maotan-Banshiling belt on the south bank. Both of them consist of
syenite, quartz-syenite and alkali feldspar granite, which were formed at about 125 Ma ago and are enriched in alkalies and
high-field-strength elements but depleted in water, with the total alkali accounting for 9–12%. and H2O+ only for 0.50%. The Ga× 10−4/Al ratio is as high as 2.7 to 3.8 for granite. They were formed in the extension stage of ancient rifting. So they are considered
to be the A-type syenite-granite belts. Granites in the two belts resulted from a syenite magma by an AFC mechanism while
the magma was derived from alkali basalt magma through the fractional-crystallization-dominated AFC mechanism.
Financially supported by the National Eighth-Five-Year Science and Technology Breakthrough Project No. 85-901-03-04. |
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Keywords: | A-type syenite-granite Anhui |
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