orogenic phase

Rock finite strain and estimation of deformed components of structural blocks in an orogenic belt;

岩石有限应变与造山带构造块体变形要素的估算

Progress in the study of the Early Paleozoic Kunlun orogenic belt;

昆仑早古生代造山带研究进展

Tectonic facies along the Nujiang-Lancangjiang-Jinshajiang orogenic belt in southwestern China;

西南“三江”造山带大地构造相

Mesozoic asthenospheric upwelling orogeny in eastern China;

中国东部中生代软流层上涌造山作用

Research Advances in Erosion,Rheology of the Lower Crust and Orogeny;

地表剥蚀、下地壳流变与造山作用研究进展

Evidence of magmatic petrology for the Yanshanian orogeny in the Dabie oroge n;

大别造山带燕山期造山作用的岩浆岩石学证据

Following the Indosinian movement, intensive intracontinental orogenesis occurred in the Qinling orogenic belt due to the joint effects of the three great tectonic domains of Paleo-Asiatic,circum-Pacific and Terthyan tectonics,which formed the basic tectonic framework of structural schist system with interfingering banded and massive structrues in this area.

印支运动后的秦岭造山带受古亚洲构造域、环太平洋构造域和特题斯三大构造域联合作用,发生了强烈的陆内造山,奠定了该区条块相间构造岩片系统的基本构造格架,控制了本区斑岩型钼矿和众多热液型多金属矿产的最终成矿作用和矿带展布。