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    Volume 31 Issue 1
    Jan.  2006
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    Article Contents
    SUN Qian, FAN Qi-cheng, LONG An-ming, YIN Ke-jian, 2006. Nanwan Volcano Eruption Features on Weizhou Island, Guangxi. Earth Science, 31(1): 66-70.
    Citation: SUN Qian, FAN Qi-cheng, LONG An-ming, YIN Ke-jian, 2006. Nanwan Volcano Eruption Features on Weizhou Island, Guangxi. Earth Science, 31(1): 66-70.

    Nanwan Volcano Eruption Features on Weizhou Island, Guangxi

    • Received Date: 2005-12-03
    • Publish Date: 2006-01-25
    • Weizhou island is a volcanic island, which is located in Beibu Bay. The base of Weizhou island is constituted by lava. The Nanwan volcano effusive mass forms modern volcanic physiognomy of Weizhou island. Pycroclastics and base surge extend to the north island, covering more than half of the island. Eyuzui and Zhuzidao are two typical sections, which are selected in order to observe and describe the volcanic activity of Nanwan volcano in detail. Special structures were found that belong to the base surge, including large-scale and low-angle cross-bedding, slaty-bedding, climb-bedding, and distal facies accretionary lappili. These structures prove that Nanwan volcano is a multiplex volcano caused by alternation of magma eruption and phreatomagmatic eruption. Phreatomagmatic eruption plays an important role in the formation of Nanwan volcano. The eruptive center is located in the Nanwan sea.

       

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