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浙江中生代火山构造
引用本文:水涛.浙江中生代火山构造[J].地质科学,1981,0(2):113-121.
作者姓名:水涛
作者单位:浙江省地质科学研究所
摘    要:浙江省十余万平方公里面积中,三分之二为中生代(上侏罗世及白垩纪)陆相火山岩所被复。对此广大火山岩区开展区域火山构造研究有重要意义。但至今在火山岩区大都还是沿袭沉积岩覆盖区的工作方法,停留在火山活动期后线形构造的调查和分析。

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收稿时间:1979-08-01
修稿时间:1979-08-01;

RESEARCHES ON MESOZOIC VOLCANIC STRUCTURE IN ZHEJIANG PROVINCE
Shui Tao.RESEARCHES ON MESOZOIC VOLCANIC STRUCTURE IN ZHEJIANG PROVINCE[J].Chinese Journal of Geology,1981,0(2):113-121.
Authors:Shui Tao
Institution:Zhejiang Institute of Geology, Hangzhou
Abstract:This paper deals with the problems pertaining to the methodology of regional volcanic structure,and put forward an approach to the methodology with the study of volcanic structural traces as starting point combined with regional geology,geophysical field and geochemical circumstances.Following such a way the author of this paper made researches on the general features and laws of the volcanic structure of continental facies,expounds the restrictive relationship between the regional horizontal stress field and point vertical stress field under the action of volcanic magma,and analysed the framework structure of volcanic basement.Besides,based upon some geological data of strontium isotope,this paper also disucsses the origin of volcanic substance and its relation with regional geotectonies.
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