摘要
秦皇岛北部山区属燕山山脉的东段,在大地构造上处于华北地台的北缘,东邻太平洋板块,紧靠郯庐大断裂,各类地质作用活跃,地质遗迹资源丰富。区内保存了从新太古代至新生代30亿年以来各个地质历史时期形成的地层单位。沉积作用、岩浆作用、火山活动以及各类变质作用的遗迹均有保留,岩石类型齐全,矿物种类丰富,是研究华北地台海陆变迁、气候演化的重要资料和依据,具有很高的科学研究、科普和教学价值。秦皇岛面向渤海,受东南海洋季风和海洋暖流的影响,气候湿润,森林覆盖率高,动植物资源丰富,是草原文化与农耕文化的交融区,人文资源丰富。该区集地质遗迹、奇峰、峡谷、瀑布、溪流、生态和人文资源于一体,具有建设大型地质公园的天然资源。
The northern mountainous area of Qinhuangdao belongs to the eastern section of Yanshan mountains, tectonically located in the northern margin of North China Platform, adjacent to the Pacific plate in the east, close to the Tanlu fault. And various types of geological actions are active, geological heritage resources is abundant. The area saves stratigraphic units formed in each geological period from the Neoarchean to Cenozoic that a total of 3 billion years. Deposition, magmatism, volcanism and the remains of various types of metamorphism are preserved, the rock types are complete, mineral species are rich, it is an important data and basis studying on the sea changes and climate evolution of the North China platform owning high scientific research, popular science and teaching value. Facing Bohai and affected by the ocean southeast monsoon and ocean currents, the climate of Qinhuangdao is moist, the forest coverage rate is high, the animal and plant resources are rich. Qinhuangdao is a blend of grassland culture and agricultural culture, and it owns rich human resources. In the area, the geological relics, ecological and human resources are in one, and there are natural resources to build a large geological park.
引文
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