1)  apo orogenic intrusion
造山期后侵入作用
2)  apoorogenic intrusion
造山期后侵入作用
3)  orogeny
造山
4)  orogenesis
造山
5)  weak orogeny
弱造山
6)  orogenic belt
造山带
1.
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
2.
Progress in the study of the Early Paleozoic Kunlun orogenic belt;
昆仑早古生代造山带研究进展
3.
Tectonic facies along the Nujiang-Lancangjiang-Jinshajiang orogenic belt in southwestern China;
西南“三江”造山带大地构造相
7)  orogeny
造山作用
1.
Mesozoic asthenospheric upwelling orogeny in eastern China;
中国东部中生代软流层上涌造山作用
2.
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
3.
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
8)  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。
9)  "suborogenic belt"
“次造山带”
10)  orogen
造山带
1.
Metallogeneses in the collisional orogen of the Qinghai-Tibet Plateau: Tectonic setting, tempo-spatial distribution and ore deposit types;
青藏高原碰撞造山带成矿作用:构造背景、时空分布和主要类型
2.
Nature of Main Tectono-Lithostratigraphic Units of the Qinling Orogen: Implications for the Tectonic Evolution;
秦岭造山带主要构造岩石地层单元的构造性质及其大地构造意义
3.
Dabieshan Mountain orogen consisted of the south-east Qinling fold Zone,controls the magmatic rock together in southern Henan Province with Guishan-Meishan fault zone and north-east fault.
大别山造山带,是秦岭褶皱带南东的组成部分,它与龟(山)—梅(山)断裂带、北东向断裂共同控制着豫南岩浆岩的分布。
补充资料:阿尔卑斯造山带
欧洲的阿尔卑斯以及其它一些年青的巨大造山带和褶皱山系。早第三纪和晚第三纪由于阿尔卑斯运动(中国称喜马拉雅运动),使沿欧洲南部中生代的古地中海发生了强烈褶皱,形成横贯东西的阿尔卑斯-喜马拉雅山脉(从西班牙至亚洲南部)。严格地说,此词只限于造山带的北翼,由徐士(E.Suess)创名。同义词有“地中海带”、“阿尔卑斯-喜马拉雅带”。板块构造学说认为,这个造山带属碰撞型山链。(共213字)

【引用信息】徐世芳,李博主编.地震学辞典.北京:地震出版社.2000.第5页.
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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