| 浙闽沿海壳幔同位素演化轨迹研究 |
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| 关键词:isotopic evolution partial melting Zhejiang and Fujian |
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| CRUST-MANTLE ISOTOPIC EVOLUTION TRACK ALONG THE MARGIN OF THE PACIFIC IN ZHEJIANG AND FUJIAN PROVINCE |
| The Sr-Nd-Pb isotope evolution in the investigated area appear in a clear track.The isotopic char-acteristics of magmatic rocks in the uplifted area are derived from partial melting or remelting contami-nation of Proterozoic continents in the lower crust.Large guantity of the Mesozoic volcanic eruption in the area nearer to the pacific was caused by the mantle upwelling.The Sr-Nd-Pb isotopic compeition of the volcanic rocks has a characteristics of crust-mantle hybridization,that can be revealed from the ewist of isotopic evolution track. |
| YING Jun-long,ZHAO Pu-yun,ZHANG Hong,GUO Hong.1994.CRUST-MANTLE ISOTOPIC EVOLUTION TRACK ALONG THE MARGIN OF THE PACIFIC IN ZHEJIANG AND FUJIAN PROVINCE[J].Acta Geoscientica Sinica,15(1,2):68-74. |
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