山东烟台招虎山地质遗迹特征及综合评价

Characteristics and Comprehensive Evaluation of Geological Relics in Zhaohushan Mountain in Yantai City in Shandong Province

摘要:

招虎山属于崂山山系的分支，形成时代为中生代燕山运动晚期，主要岩性为细粒二长花岗岩和正长花岗岩，地质遗迹类型共分地质（体、层）剖面、地质构造、地貌景观、水体景观和环境地质遗迹景观5个大类、7个类、9个亚类。本文分析了地质遗迹的成因、形态及规模等，并对其进行了科普、观赏、旅游开发3个方面的综合评价，招虎山地质遗迹种类繁多、地学信息量丰富、地质内涵深隧，地学科普旅游潜在巨大的价值，合理开发招虎山地质遗迹资源，可能为当地带来显著的社会效益和经济效益。

Abstract:

Zhaohushan mountain belongs to the branch of Laoshan mountain system. It was formed in the late Mesozoic Yanshan movement. The main lithology is fine-grained monzogranite and syenogranite. The types of geological relics are divided into 5 large categories, 7 categories and 9 subcategories, they are geological (body and layer) profile, geological structure, geomorphic landscape, water landscape and environmental geological relics landscape. In this paper, the causes, forms and scale of geological relics have been analyzed, and a comprehensive evaluation has been made from science popularization, viewing and tourism development. Zhaohushan mountain has a wide variety of geological relics, rich geoscience information, deep geological connotation and great potential value of geoscience science popularization tourism. Rational development of geological relics resources in Zhaohushan mountain may bring significant social and economic benefits.