极地研究

极地研究 ›› 1996, Vol. 7 ›› Issue (1-English): 1-18.

• 目次 •    下一篇

Self-organization phenomena of the nonequilibrium process in magmatism of the Fildes Peninsula, West Antarctica

 Li Zhaonai, Li Hansheng and Shang Ruxiang   

  1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
  • 出版日期:1946-03-30 发布日期:1946-03-30
  • 通讯作者: Li Zhaonai

Self-organization phenomena of the nonequilibrium process in magmatism of the Fildes Peninsula, West Antarctica

 Li Zhaonai, Li Hansheng and Shang Ruxiang   

  1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
  • Online:1946-03-30 Published:1946-03-30
  • Contact: Li Zhaonai

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摘要：

Volcanic geological,petrological and geochemical characteristics of the Tertiary volcanic rocks from the Fildes Peninsula,West Antarctica show that magma evolution was a process of dissipation of heat energy exchanged energy and mass occurring between the magma system and its surrounding environments, and with the feature of dynamic equilibrium and periodicity(stage). In the study volcanic rocks of different types commonly exhibit a multi-grade composite texture and the derivative magmas produced by differentiation of parent magymas in the magma chamber show a zonal structure in the high--level--magma chamber which represent self-organization phenomenon of the nonequilibrium process in magmatism. The self-organization phenomenon is dissipative structure formed under given conditions.

关键词: West Antarctica, Fildes Peninsula, magmatism, self-organization phenomenon

Abstract:

Volcanic geological,petrological and geochemical characteristics of the Tertiary volcanic rocks from the Fildes Peninsula,West Antarctica show that magma evolution was a process of dissipation of heat energy exchanged energy and mass occurring between the magma system and its surrounding environments, and with the feature of dynamic equilibrium and periodicity(stage). In the study volcanic rocks of different types commonly exhibit a multi-grade composite texture and the derivative magmas produced by differentiation of parent magymas in the magma chamber show a zonal structure in the high--level--magma chamber which represent self-organization phenomenon of the nonequilibrium process in magmatism. The self-organization phenomenon is dissipative structure formed under given conditions.

Key words: West Antarctica, Fildes Peninsula, magmatism, self-organization phenomenon