SGER: An Exploratory Study of Surface Wave Dispersion in the Indian Ocean, Indian Subcontinent and Western China

SGER：印度洋、印度次大陆和中国西部面波色散的探索性研究

• 批准号: 0342931
• 负责人: Francis Wu
• 金额: $ 2.64万
• 依托单位: SUNY at Binghamton
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2003
• 资助国家: 美国
• 起止时间: 2003-09-15 至 2005-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0342931&HistoricalAwards=false
• 关键词: SGER; Exploratory; Study; Surface; Wave

Two of the world's first order geophysical features are found in India and its surrounding areas. First, the Himalaya and the Tibetan plateau are by far the most outstanding topography of the Earth; based on all available evidence it is known that the northward motion of the Indian subcontinent is the root cause that led to its formation. But what were the geological processes in the interior of the Earth in this area as the subcontinent plowed northward? Furthermore, in the geoidal map of the world, the Indian Ocean basin and southern India area is marked by the largest low anomaly. This geoidal low implies that there is a relative mass deficiency under the area, but at what depth and how much? Why did it form? The mechanisms that led to their formation most probably left traces in the crust and mantle under this area. A detailed mapping of the crust and upper mantle is therefore the first step toward understanding the processes. Only recently data from high quality portable seismic stations and a permanent network came into existence and data from these networks have accumulated to a degree when significant analyses can be preformed. The proposed work here will be performed in cooperation with Dr. S.S. Rai of National Geophysical Research Institute (NGRI), Hyderabad, India. We plan in the short term to use surface waves to image the lateral variations as well as resolution of upper mantle (down to ~300 km) structures. Our longer-range plan is to conduct a comprehensive surface wave tomographic study of the area.

在印度及其周边地区发现了世界上两个一级地球物理特征。 首先，喜马拉雅山和青藏高原是迄今为止地球上最突出的地形;根据所有现有证据，印度次大陆向北运动是导致其形成的根本原因。 但是，当次大陆向北移动时，这一地区的地球内部发生了什么地质作用呢？ 在世界大地水准面图上，印度洋海盆和印度南部地区是最大的低异常区。 这个大地水准面低意味着该地区下面存在相对质量不足，但在什么深度和多少？ 为什么会形成？ 导致其形成的机制很可能在该地区的地壳和地幔中留下了痕迹。 因此，对地壳和上地幔进行详细的测绘是理解这些过程的第一步。 直到最近才有了高质量便携式地震台站和一个永久性网络的数据，这些网络的数据积累到了可以进行重要分析的程度。 此处拟定的工作将与Dr. S.S.合作进行。印度海得拉巴国家地球物理研究所（NGRI）的Rai。 我们计划在短期内使用面波成像的横向变化以及上地幔（下至~300公里）结构的分辨率。 我们的长期计划是对该地区进行全面的表面波层析成像研究。