本文提出了构造成矿作用动力学研究的递增应力流变学方法。
An incremental stress rheology model is developed to study the dynamics of tee-tonic mineralization.
对小秦岭金矿田的成矿时代、成矿深度、矿床成因等地质问题，给出了构造地质学方面的判据。
Aiming at the metallogenic epoch, metallogenic depth and the genesis of the deposit in Xiaoqinling gold field, the evidence of tectonic geology is given out.
稳定同位素测年信息，是深部构造、成矿作用和地层年代学的重要依据。
The information of stable isotopic aging is the important basis for the deep structures, mineralization and chronostratigraphy.
深部构造与成矿作用关系的深入研究是矿床地质学目前研究工作的前沿课题和今后的发展趋势。
Research on the relationship between deep rooted structural discontinuities and giant ore deposits is the latest development in economic geology.
本文提出了构造成矿作用动力学研究的递增应力流变学方法。
An incremental stress rheology model is developed to study the dynamics of tectonic mineralization.
[8]滕吉文。地球深部物质和能量交换的动力过程与矿产资源的形成[J]。大地构造与成矿学，2003,27 (1)：3 ~21。
Teng J W. Dynamic process of substance and energy exchanges in depths of the earth and formation of mineral resources [J]. Geotectonica et Metallogenia, 2003, 27 (1) : 3 ~ 21.
[8]滕吉文。地球深部物质和能量交换的动力过程与矿产资源的形成[J]。大地构造与成矿学，2003,27 (1)：3 ~21。
Teng J W. Dynamic process of substance and energy exchanges in depths of the earth and formation of mineral resources [J]. Geotectonica et Metallogenia, 2003, 27 (1) : 3 ~ 21.
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