地震地质 ›› 2012, Vol. ›› Issue (4): 739-742.DOI: 10.3969/j.issn.0253-4967.2012.04.016

• 火山灾害与火山机理 • 上一篇    下一篇

长白山天池火山顶部黄色物质成因的初步探讨

尹功明, 樊祺诚   

  1. 中国地震局地质研究所, 地震动力学国家重点实验室, 北京 100029
  • 收稿日期:2012-10-31 修回日期:2012-11-15 出版日期:2012-12-30 发布日期:2012-12-28
  • 基金资助:

    国家自然科学基金(41272088)资助

A PRELIMINARY STUDY OF THE ORIGIN ABOUT THE YELLOW MATERIAL AT CHANGBAISHAN TIANCHI VOLCANO

YIN Gong-ming, FAN Qi-cheng   

  1. State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China
  • Received:2012-10-31 Revised:2012-11-15 Online:2012-12-30 Published:2012-12-28

摘要:

长白山天池火山是中国著名的火山,全新世以来有过多次喷发。在长白山天池火山顶部局部地区发育1套黄色碎屑物质。但是,对于这套黄色物质的成因,一直存有争议。根据1980年5月18日美国圣海伦斯火山喷发的研究成果,以及长白山天池火山顶部黄色物质的化学成分、产出特征等,我们初步推测其成因为 "千年喷发"时热水交代作用的产物,而不是一次独立的火山喷发事件的产物。

关键词: 长白山天池火山, 黄色物质, 成因, 热水交代作用

Abstract:

The Changbaishan Tianchi volcano is one of the most famous volcanoes in China. It erupted many times in the Holocene time. The top of this volcano is regionally covered by some yellow material (pyroclastics), the origin of which has been under debating since its discovery. Based on the information provided by the eruption of Mount St Helens of USA on May 18th, 1980, in conjunction with the chemical composition and distribution characteristics of the yellow materials, we estimated that it resulted from hot water metasomatism during the Millennium eruption, rather than a separate product of an individual volcanic event.

Key words: Changbaishan Tiahchi volcano, yellow material, origin, hot water metasomatism

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