地球科学进展 ›› 1996, Vol. 11 ›› Issue (1): 62 -64. doi: 10.11867/j.issn.1001-8166.1996.01.0062

新学科·新技术·新发现 上一篇    下一篇

一门新兴地质学科——流体地质学
徐学纯   
  1. 长春地质学院地质系 长春 130061
  • 收稿日期:1995-05-11 出版日期:1996-02-01
  • 通讯作者: 徐学纯,男,1954年2月出生,教授,现主要从事变质岩石学方面的研究。
  • Received:1995-05-11 Online:1996-02-01 Published:1996-02-01


[1] Walther J V,Wood B J(eds). Fluid-rock infractions during metamorphism. Springer-Verlag. New York, Berlin, Heidelberg. Tokyo,1986. 1-212.

[2] Bridgwater D (eds). Fluid movements-element transport and the composition of the deep crust. Kluwer Academic Publishers,1989. 1-394.

[3] Newton R C,Smith J V and Windley B F. Carbonic metamorphism, granulates and cruatal growth. Natrue,1980,288:45-50.

[4] Forst B R and Frost C D. CO2 melts and granulate metanorphiam. Nature,1984.327:503-506.

[5] Torgersen T. Crustal-scale fluid transportsmagnitude and mechanisms. Geophys Rea Lett,1991.18 (5):917-986.

[6] 肖庆辉等.推进我国地质科学前沿研究的谋划.北京:地质出版社,1994.

[7] Holliater L S and Crawford M L (eds). Short course in fluid incluaionsapplicstion to petrology. Min Assoc Canada.Calgary,1981.

[8] Roedder E. Fiuid inclusions. Reviews in Mineralogy 12. Mineral Soc America,1984.

[1] 蔡祖煌 石慧馨. 地震水文地质学[J]. 地球科学进展, 1992, 7(1): 90-.
阅读次数
全文


摘要