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1.
Genetically, they are the transition between I-type and S-type granites, formed in the tectonic environment of late orogenic epoch, directly related to the South Mongolian compound orogeny.
它们均形成于造山晚期构造环境,与南蒙古复合造山作用有直接关系。
2.
Orggenic Processes of the Inner Mongolia-Yanshan Area in Eastern China during the Late Late Paleozoic-Mesozoic;
中国东部内蒙—燕山地区晚古生代晚期—中生代的造山作用过程
3.
Fengshanian stage
凤山阶-晚寒武世晚期
4.
TECTONIC EVOLUTION OF THE LATE ARCHEAN WUTAISHAN COLLISION OROGEN
五台山晚太古代碰撞造山带构造演化
5.
(5) Middle and late Himalayan movements determined the formation and development of structural traps.
(5 )喜山运动中晚期活动控制构造圈闭的形成和发展 ;
6.
Geochemistry and Tectonic Setting of Early Late Paleozoic Felsic Volcanic Rocks from the Altai Orogenic Belt,North Xinjiang
阿尔泰晚古生代早期长英质火山岩的地球化学特征及构造背景
7.
There was an orogenic belt called the Cathaysian continental marginal orogenic belt in late Mesozoic along the present northern margin of the South China Sea.
南海北部陆缘在中生代晚期曾形成宏伟的华夏陆缘造山带。
8.
Late Mesoproterozoic to Paleozoic tectonothermal events in the Eastern Segment of the Central Tianshan Tectonic Zone of Northwestern China:Constraints from SHRIMP zircon geochronology.
中天山东段中元古代晚期—古生代构造-热事件:SHRIMP锆石年代学证据
9.
The west zone of volcanic rock petrographic province in late Mesozoic in Fujian, Zhejiang, Jiangxi, and guangdong province can be divided into Jiangnan, Wuyi and Nanling tectonomagmatic activity regions.
将闽浙赣粤中生代晚期火山岩西区带分为江南区、夷区和南岭区三个构造—岩浆活动区。
10.
alpine age orogeny
阿尔卑斯期造山运动
11.
South Tianshan: a Late Paleozoic or a Triassic orogen?
南天山:晚古生代还是三叠纪碰撞造山带?
12.
METAMORPHISM EVOLUTION OF THE LATE ARCHEAN COLLISION OROGENIC BELT IN WUTAISHAN
五台山晚太古代碰撞造山带的变质作用演化
13.
Properties and Tectonic Environments of Late Devonian Volcanic Rocks in Akenawa Hills, Xinjiang
新疆阿克纳瓦山晚泥盆世火山岩及其构造环境
14.
THE STUDY ON THE RED SOIL OF NEOGENE IN XIAN AND BAODE OF SHANXI
西安、山西保德第三纪晚期红土的研究
15.
GEOCHEMICAL CHARACTERISTICS OF GRANITES OF LATE YANSHANIAN STAGE IN EAST ZHEJIANG
浙东燕山晚期花岗岩的地球化学特征
16.
A NEW BRONTOTHERE FROM LATE MIDDLE EOCENE OF QUFU, SHANDONG
记山东曲阜中始新世晚期─雷兽新属种
17.
NEW ADVANCES IN THE STUDY OF LATE NEOGENE STRATIGRAPHY IN THE LLIANG MOUNTAIN
吕梁山地区新近纪晚期地层研究进展
18.
Characters of Later Jurassic Yinshan Intraplate Orogeny Belt--Evidence from Daqing Shan,Inner Mongolia
阴山晚中生代板内造山特征及其动力机制——以内蒙古大青山为例