1) Intracontinental basin-range orogenesis of diwa type
地洼型陆内块断造山
2) diwa type orogeny
地洼型造山
3) diwa-type orogeny
地洼型造山运动
1.
The author define the diwa-type orogeny in the frame of diwa theory as the collection of geological processes wlthin post-platformal tectono magmatism, and then divide it by the manifestations and dynamics of crustobody into three sub-types, convergent, divergent and hybrid diwa-type oro.
笔者将地洼型造山运动定义为在后地台构造-岩浆活化过程中各种地质作用的总称，并且依据壳体运动的方式和力源，可以将地洼型造山运动划分为离散式、汇聚式和混合式三类。
4) 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。
5) 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
6) volcanic tectonic depression
火山构造洼地
1.
Volcanic eruptive belts from Ningguo to Cuomai is divided into two volcanic tectonic depression including Ningguo and De.
根据区域构造背景、火山岩地层时空分布特征、岩性、岩相及喷发形式,将研究区划分为三个火山喷发带,其中宁果—措麦火山喷发带又可划分为宁果和德诺两个火山构造洼地,卢当—查孜火山喷发带划分为孔隆—邦勒、松拉勒—腊尔格和孔驹密波—查孜三个火山喷发亚带。
补充资料：地内
【地内】
（杂名）(参见：地中)
（杂名）(参见：地中)
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