Monitoring of active deformation of the Hengchun Peninsula in southern Taiwan using Persistent Scatterer Interferometry

摘要：

The island of Taiwan is the result of the ongoing collision between the Philippines Sea Plate and the Eurasian Plate with a high rate of convergence of about 8.2 cm/yr.The Hengchun peninsula in the southern tip of the Taiwan Central Range is the least deformed and the most complete accretionary prism sequences as a result of oblique collision of the Taiwan orogeny.Several studies based on palaeostress, radiocarbon dating, GPS and precise leveling have been done about this fault but no using space geodesy such as Synthetic Aperture Radar Interferometry (InSAR).

作者: 胡植慶

会议类型: 国内会议

会议名称: 南海资源环境与海疆权益学术研讨会、第十五届海峡两岸地貌学研讨会暨中国第四纪研究会海岸海洋专业委员会、中国地理学会海洋地理专业委员会2014联合学术年会

会议地点: 南宁

会议语种:英文

页码: 66-66

在线出版日期: 2014-07-18（万方平台首次上网日期，不代表论文的发表时间）