Lithogeochemistry of volcanic rocks and hosted melt inclusions in Wudalianchi, Heilongjiang, China

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• 作者：Ni Li (1)
  Qicheng Fan (1)
  Qian Sun (1)
  Rubo Sun (2)
  
• 关键词：Wudalianchi volcanic rock ; Laoheishan volcano ; Huoshaoshan volcano ; melt inclusion
• 刊名：Journal of Earth Science
• 出版年：2009
• 出版时间：October 2009
• 年：2009
• 卷：20
• 期：5
• 页码：771-783
• 全文大小：877KB
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• 作者单位：Ni Li (1)
  Qicheng Fan (1)
  Qian Sun (1)
  Rubo Sun (2)
  
  1. Institute of Geology, China Earthquake Administration, Beijing, 100029, China
  2. Wudalianchi Earthquake and Volcano Observatory, Heilongjiang Earthquake Administration, Wudalianchi, 064005, China
  
• ISSN：1867-111X

文摘

Wudalianchi () volcanoes are famous Quaternary ones with fairly good volcanic landscape in Northeast China. The volcanic rocks are phonotephrite, tephri-phonolite, trachyandesite, and basaltic trachyandesite with SiO2 contents of 47.3 wt.%-4.2 wt.%. The characteristic of high K2O content in Wudalianchi volcanic rocks suggests that they probably share a common potassic magma source. The magma evolutions of Wudalianchi volcanic rocks are similar, while the new eruption products of Laoheishan ( and Huoshaoshan ( volcanoes are slightly more evolved than the old eruption materials, i.e., the magma of the new eruptions in 1719-721 from the above two volcanoes is the evolved magma in underground chamber. The main phenocrysts of Wudalianchi volcanic rocks are olivines, clinopyroxenes, and some characteristic K-rich leucites. The various-shaped melt inclusions are found in olivine phenocrysts from new eruption products of Laoheishan and Huoshaoshan volcanoes. By electron microprobe (EMP) analyzing, the contents of SiO2 and total alkali show a wide range, suggesting that the pre-eruptive magma was probably more complicated, or the melt inclusions were rather unhomogeneous. On the basis of EMP results, it is believed that the sulfur degassing rate from this new eruption was much higher than that of the millennium eruption of Tianchi () volcano, while the chlorine degassing rate was a magnitude lower than that of Tianchi volcano.