摘要
经过野外考察和室内光弹实验等测试表明，香港地区岛屿的形成与演变机制，是 以断裂构造为基础，海陆变迁为动力。形成的年代是全新世中期大温暖期高海面。
Conditions for the formation of islands in the Hong kong area were basically fault construction. With the rise of sea level, merged land became islands. The process lasted from the neo-Pleistocene Epoch through the warm period of the Mid-Holocene Epoch when the sea level rose. This finds evidence not only in light elastic experiment in the lab but also in 14C analysis.
出处
《海洋科学》
CAS
CSCD
北大核心
1999年第1期61-64,共4页
Marine Sciences
关键词
香港
断裂构造
海陆变迁
岛屿
形成
演变
Fault construction
^(14)C dating
Light elastic experiment
Sea-land changes
Hong Kong
