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1)  intracontinental orogeny and basin-forming
陆内造山成盆
2)  basin-making of continental interior
陆内造盆
3)  intracontinental orogenesis
陆内造山
1.
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。
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4)  intracontinental orogeny
陆内造山
1.
Deep-seated factors controlling the intracontinental orogeny of Yanshan Mountains.;
燕山陆内造山作用的深部制约因素
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5)  intracontinental orogenic zone
陆内造山带
1.
Stratigraphy of Mesozoic and Cenozoic intracontinental orogenic zones: an example from the Yanliao orogenic zone;
中新生代陆内造山带的地层学研究———以燕辽造山带为例
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6)  Yanshan intracontinental orogenic belt
燕山陆内造山带
1.
Panshan granitoid pluton situated in the southern margin of middle segment of Yanshan intracontinental orogenic belt consists of four intrusive units (Langjiayu,Guanzhuang,Dongluozhuang,Xiaopanshan) and porphyritic quartz-monzonite veins.
位于燕山陆内造山带中段南缘的蓟县盘山花岗岩体由狼家峪、官庄、东罗庄和小盘山4个侵入单元组成,并发育侵入期后含斑石英二长岩脉,发育环绕岩体分布的周缘向斜并侵蚀早期东西向蓟县断裂。
补充资料：成造
1.造就。 2.制造。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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