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大陆地质学研究的若干问题思考

陈国能   

  1. 中山大学地球科学系
  • 收稿日期:1997-09-20 修回日期:1997-09-20 出版日期:1997-09-20 发布日期:1997-09-20

PONDERING OVER SOME PROBLEMS IN THE STUDY OF CONTINENTAL GEOLOGY

Chen Guo-neng   

  1. Department Geology, Zhongshan, Guangzhou 510275
  • Received:1997-09-20 Revised:1997-09-20 Online:1997-09-20 Published:1997-09-20

摘要: 板块说阐明了洋壳的物质循环,而地槽说则阐明了地壳表层的物质循环,两者之间显然尚欠缺一个关于大陆内部的物质演化模型,因此,要建立大陆地质学的系统理论, 无应该查明大陆内部的物质过程;而建立大陆内部物质化模型的关键,是阐明组成大陆地壳重要部分的花岗岩的成因,传统的岩浆侵入式无法容纳与花岗岩有关的各种资料,在地温场状态上的将今论古是花岗岩成因研究中的思维误区。

Abstract: Plate Tectonics has expounded the material cycle of oceanic crust, and Geosyncline Theory has done that of earth’s surface. Thus a model about the material evolution in continental interior is the necessity for establishing systematic theory of continental geology, and the key to the model is to clarify the genesis of granite which constitutes an important part of the continental crust. The traditional magmatic intrusion hypothesis is not able to hold various data concerning granite. It is a thinking fallacy for the research of granite genesis to use the method of “taking the present as the key to the past” in status of geothermal field.