| 1. | Thailand indochina policy in chatichai era
也论差猜时期泰国的印支政策 |
| 2. | On domestic studies of indo - china peace restoring issue of geneva conference in
国内对1954年日内瓦会议恢复印支和平问题的研究 |
| 3. | On the current situation and prospecats of burmese and indo - chinese countries ' economic development
缅甸和印支国家经济发展的现状与前景 |
| 4. | 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 |
| 5. | Indosinian nappe structure and its hydrocarbon significance in hefei basin and north huaiyang tectonic zone
合肥盆地与北淮阳构造带印支期的推覆构造及其油气意义 |
| 6. | 7 . the dabie orogenic belt is of transformation and superposition character . its new superimpose
Ne向郯庐断裂系的大型平移作用叠加在原来印支期消减带之上，产生新的俯冲。 |
| 7. | The basement uplift , the platform shallowening and the marine regression have close relations with the indosinian movement
古地理演化是构造运动的直观响应，中国南方三叠纪的地壳抬升、台地浅滩化、海水退出与印支运动密切相关。 |
| 8. | The coi - rich " inclusions and normal nacl + h2o inclusions are commonly observed in same samples with the same homogenization temperature ( th ) . 4
Ar - ar同位素地球化学研究表明，萨瓦亚尔顿金矿床的主要成矿时代为印支晚期， 210ma 。 |
| 9. | The first is the depression karst development pattern from dissolution of karst hill during indo - chinese epoch which is the key period for forming space of the reservoir
其中印支早燕山期裸露岩溶属溶丘（梁）洼地型岩溶发育模式，是储集空间形成的重要时期。 |
| 10. | Camp belong to the south qinling orogenic belt middle segment palaeozoic strench basin fold indo - chinese epoch drape north part , and belong to the miliangchuan schiefer
矿区所在部位属南秦岭造山带中带古生代伸展盆地叠加印支期冲褶带的北部，隶属于米粮川逆冲岩片。 |
