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| 试论上海及邻区晚新生代沉积特征与断裂构造的关系 | |
| 引用本文： | 顾志文. 试论上海及邻区晚新生代沉积特征与断裂构造的关系[J]. 华东师范大学学报(自然科学版), 1997, 0(2): 68-75 |
| 作者姓名： | 顾志文 |
| 作者单位： | 华东师范大学地理系!上海，200062 |
| 摘 要： | 本文阐述了上海及邻区晚新生代沉积相的分布特征。根据晚新生代沉积等厚线走向分析了沉积厚度与断裂构造的关系，尤其是沉积厚度较大的地区及几个沉积中心与北西向断裂的关系。 |
| 关 键 词： | 晚新生代 沉积厚度 断裂构造 新构造运动 沉积相 |
On the Relationship between Sedimentary Feature and Faulted Structure of Upper Cenozoic Group in Shanghai and Its Adjecent Regions |
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| Gu Zhiwen. On the Relationship between Sedimentary Feature and Faulted Structure of Upper Cenozoic Group in Shanghai and Its Adjecent Regions[J]. Journal of East China Normal University(Natural Science), 1997, 0(2): 68-75 | |
| Authors: | Gu Zhiwen |
| Abstract: | This paper deals with the distribution feature of Late-Cenozoic sedimentary factes inShanghai and its adjecent regions. Based on the isopach map of Late-Cenzoic sediments, the relationship between the sediment phickness and faulted structure is studied. In particularly, several areas with thicker sediments relative to NW-orieted fault system are also discussed. |
| Keywords: | late-cenozoic era isopach map sediment thickness |
| 本文献已被 CNKI 维普 等数据库收录！ | |