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1)  continental margin orogenesis
陆缘造山
2)  continental margin orogenic zone
陆缘造山带
3)  continental-margin orogenic belt
大陆边缘造山带
1.
According to the tectono-geomorphological features and characteristics of neotectonic movement on the southwestern margin of the North American continent,the author has established a 3D tectonomechanic model of the reversed S-shaped continental-margin orogenic belt of the northern hemisphere.
文中根据北美大陆西南边缘造山带的构造地貌及新构造运动特征,建立了反S状大陆边缘造山带的三维构造力学模式,指出阿拉斯加地区为弧形右旋剪切隆升造山带;科迪勒拉造山带为直线右旋走滑造山带;马德雷山以南,延至加勒比海为一左旋沉降‘旋扭沟-弧-盆系统’。
4)  pericontinental tectonic framework
陆缘构造
5)  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。
6)  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
补充资料:山缘草碱
分子式:
CAS号:

性质:又称紫罂粟碱。(-)旋体,六方形片状结晶(氯仿-甲醇)。熔点180℃。旋光度 -42.5 (c=0.8,氯仿)。(±)旋体,粗短棱柱结晶。熔点190℃。存在于罂粟科植物蕈状山缘草[Adlumia fungosa Greene (A.cirrhosa Kom.non Raf.)],条裂紫堇(Corydalis lineariodes Maxim.)中。有兴奋子宫作用。

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