| 1. | Large stack deposits are controlled by deeply dipping faults tertiary age .
巨大的堆型矿体受第三纪倾陡断层控制。 |
| 2. | Extreme climates events in the cretaceous and paleogene
白垩纪至早第三纪的极端气候事件 |
| 3. | Early tertiary fossil plants and paleoclimate of lanzhou basin
兰州盆地早第三纪植物及古气候意义 |
| 4. | Sr isotope ' s analysis of the paleogene of dongpu depression
东濮凹陷下第三纪锶同位素地球化学分析 |
| 5. | The tilting rotation activity of paleaogene fault block is very obvious
早第三纪断块体的掀斜旋转运动十分明显。 |
| 6. | The phytolith of later pliocene in colorful sand forest of luliang , yunnan
云南陆良彩色沙林晚第三纪地层中的植硅石 |
| 7. | Paleocene the oldest epoch of the tertiary , 65 - 55million yesrs ago
古新世：第三纪最古的年代， 6500万5500万年前。 |
| 8. | Studies of geological samples from the kt boundary revealed the presence of c60
从研究白垩纪，第三纪交接的地质样本中找到碳- 60分子。 |
| 9. | Studies of geological samples from the k t boundary revealed the presence of c60
从研究白垩纪，第三纪交接的地质样本中找到碳- 60分子。 |
