| 1. | Formed . the average crust up rate in this area from
晚更新世以来这一地区的地壳平均上升速率为0 . 200 . 28mm a 。 |
| 2. | Environmental changes since late - pleistocene in north - bank of yangtze river , nanjing
南京江北地区晚更新世以来环境演变研究 |
| 3. | Preliminary study on late pleistocene phreato - magmatic eruptions in northern hainan island
琼北地区晚更新世射气岩浆喷发初步研究 |
| 4. | The radiocarbon ages of charcoal and their implication derived from ciergou site along the haiyuan strike - slip fault
永定河上游晚更新世晚期以来的堆积阶地年代测定 |
| 5. | The discovery and its significance of late quaternary involution in the area of lower reach of qingshuihe river , ningxia , china
宁夏清水河下游晚更新世冰卷泥的发现及意义 |
| 6. | The eastern yantai - weihai segment is a mid pleistocene segment on which no late pleistocene offset has been found
东段烟台威海段为中更新世活动段，没有发现晚更新世地层错断现象。 |
| 7. | Optical stimulated luminescence dating of late pleistocene terrace deposits in the eastern segment of the altyn tagh fault and its tectonic implication
阿尔金断裂带东段晚更新世阶地沉积物红外释光测年及其构造意义 |
| 8. | There were three times of sea - level fluctuation corresponding to the paleo - climate evolution , which had formed the sediments of alternative sea and river facies
晚更新世以来的三次海平面升降变化造成了潍河下游地区海陆沉积环境交替，形成了巨厚的海陆交互相沉积层。 |
| 9. | The same grade terrace height beside the river is surveyed at almost the same level , proved that the hidden fault under the river never moved after
经测量河流两侧相对应的同级阶地面处在相同的高度上，证明自晚更新世大凌河三级阶地形成以来位于大凌河床底部的隐伏断裂没有过活动。 |
| 10. | In the recent years the study on the loess - palaeosol sequence has obtained many achievements that have attracted the attention of the world , but it mainly relies on the indirect physical and chemical proxies
近年来在探索东亚更新世尤其是晚更新世的环境演化规律方面取得了令世界瞩目的成果，但其研究多采用间接理化替代性指标。 |
