1) Indochina
印支
1.
On the eve of Geneva Conference,the attitudes of major powers(Soviet Union,China,Democratic Republic of Vietnam,US,UK and France) towards the conference can be divided into three categories:the dominant attitude in socialist group is reflected in Soviet Union and China s policy,which intends to restore the peace in Indochina and to seek to reach an agreement at the Conference.
日内瓦会议前夕,苏、中、越(印支地区大国),美、英、法的会议态度可以分为三类:社会主义阵营三个国家的主导意见体现为苏联、中国的与会政策,谋求通过会议达成协议,恢复印支和平;美国坚决拒绝缓和;英、法两国持观望态度,一方面寄望于会议达成协议,另一方面又考虑如不能达成协议,即与美国一起筹划东南亚集体防御体系。
2) Indo-Chinese epoch
印支期
1.
Basin evolution and sequence stratigraphic framework of south of China during Hercynian cycle to Indo-Chinese epoch;
海西-印支期中国南方的盆地演化与层序格架
2.
Sedimentary characteristics and provenance analysis of Indo-Chinese epoch in the southwest edge of Ordos Basin;
鄂尔多斯盆地西南缘印支期沉积特征及物源
3.
Influence of Qinling Orogenic Movements in Indo-Chinese Epoch to sedimentary characteristics of Yanchang Formation in Ordos Basin;
印支期秦岭造山活动对鄂尔多斯盆地延长组沉积特征的影响
3) Indosinian movement
印支运动
1.
Discussion on the Characteristics of Indosinian Movement in Fujian Province;
关于福建印支运动性质的讨论
2.
The Indosinian movement, beginning from the mid-Jurassic to the early Jurassic, is the product of the convergence of North China and South China plate, and imposing a far greater effect on the tectonic conditions in Jiyang depression through the immense NE—SW direction stress.
三叠纪中期至侏罗纪早期的印支运动动力来源于华北板块与扬子板块的聚敛,聚敛作用形成巨大的NE—SW向挤压力首先导致济阳坳陷北西向压性构造的形成,产生了一系列NW向褶皱隆起带及其伴生的宽缓向斜,其次在对济阳盆地产生多处NW向挤压逆冲构造,伴之以褶皱构造。
4) Indosinian
印支期
1.
Important significance of regional tectonic regime to metallogenic capacity of Indosinian and Early Yanshanian granites in southeastern Hunan:A case study of Qianlishan and Wangxianling plutons;
区域构造体制对湘东南印支期与燕山早期花岗岩成矿能力的重要意义——以千里山岩体和王仙岭岩体为例
2.
~(40)Ar/~(39)Ar Isotope Dating on Muscovites from Indosinian Raremetal Depositsin Central Altay, Northwestern China;
新疆阿尔泰印支期伟晶岩的成矿年代学研究
3.
Relationship of petro-geochemical characteristics to metallogenic capacity differences between Indosinian and Early Yanshanian granites in southeastern Hunan;
湘东南印支期与燕山早期花岗岩成矿能力差异与岩石地球化学特征关系探讨
5) Middle Indo_chinese epoch
印支中期
6) Indo-China movement
印支运动
1.
Nappes are products formed in the compressional State by Indo-China movement in late Triassic Period.
推覆体是挤压环境下的产物，它形成于晚三叠世末期的印支运动。
参考词条
补充资料：印支半岛
印支半岛就是中南半岛，印度支那地区。它西临孟加拉湾、安达曼海和马六甲海峡，东、南临南海。包括越南、老挝、柬埔寨、缅甸、泰国、新加坡及马来西亚西部。面积206.5万平方千米，占东南亚面积的46％。海岸线长1.17万千米，多重要港湾。地势北高南低，多山地和高原。北部是古老高大的掸邦高原，海拔1500～2000米。众多山脉自南向北呈扇状延伸，形成掸邦高原及南部山、谷相间分布的地形格局。主要山脉自西向东依次为那加山脉、若开山脉；登劳山脉、他念他翁山脉、比劳克东山；长山山脉。3大山序之间的伊洛瓦底江、萨尔温江、湄南河、湄公河、红河自北向南，汹涌奔腾，源远流长。河流上游多穿行于掸邦高原，深切的河谷将高原分为数块，如伊洛瓦底江与萨尔温江之间的东缅高原，萨尔温江与湄公河间的清迈高原，湄公河与红河之间的老挝高原等。一些河流的中下游河谷平原及各河的河口三角洲为主要农业区和人口集中区。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。