| 1. | 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 |
| 2. | 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 |
| 3. | 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。 |
| 4. | 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。 |
| 5. | The qiongzhong granite should have been formed at orogenic relaxing stage after the peak of indosinian orogeny , and the danxian granite were formed at the latest orogenic phase
琼中岩基可能形成于“印支期”碰撞造山运动峰期后的松弛阶段，而儋县岩基则可能形成于造山运动的结束阶段。 |
| 6. | The basin was controlled by both dabie orognic belt and tan - lu fault zone . the model of the basin is a complex type that was composed of foreland and strike - slipping flexure in this period
这一系列现象表明，郯庐断裂带起源于华北与华南板块印支期的陆?陆碰撞中，以转换断层的型式出现。 |
| 7. | The pre - jurassic basement of hefei basin was composed of thrusts . indosinian foreland thrusts in pre - jurassic bedrocks of the basin increase towards the tan - lu fault zone , indicating indosinian activity of the fault zone
合肥盆地在印支期的前侏罗纪基底主要表现为大别造山带前陆逆冲推覆构造，由一系列逆冲断层和逆冲岩片所组成。 |
| 8. | The authors deduce that during late palaeozoic - indosinian period , the alxa fault block and the north china block may be located in the same geodynamic system , but the tarim block may be located in a different geodynamic system
推断阿拉善断块和华北断块在晚古生代印支期可能处于同一地球动力学体系内，而塔里木断块可能处于另一地球动力学体系。 |
| 9. | In a word , the stress field variation since mesozoic can be divided into five periods such as indosinian epoch , early yanshan epoch ( j3 - k1 ) , end of yanshan epoch , eogene , neogene and quaternary , it is mainly affected by the active pattern of tanlu large fault
综合研究认为，本区自中生代以来的应力场变化可分为印支期、早燕山期( j3 - k1 ) 、燕山末期、早第三纪、晚第三纪及第四纪五个阶段，应力场的变化主要受郯庐大断裂活动方式的影响。 |
| 10. | The strike - slip event in early cretaceous made the largest contribution to the basin was that it broke the basin pattern of foreland and strike - slipping flexure in indosinian and went into a newly nne structure pattern . this indicated that the tectonic scenario of the basin had been changed from teties structure to the pacific tectonics
该期走滑事件对合肥盆地的最大贡献在于它打破了印支期，前陆+走滑的盆地格局，而进入到一个全新的北北东向的构造格局，标志着盆地的构造背景由特提斯为主的构造域向以太平洋构造域为主的转化。 |
