隋唐宋时期浙江采石格局及其环境驱动  

The quarrying patterns and its environmental drivers in Zhejiang during Sui,Tang and Song dynasties

作　　者：朱丽东[1] 金莉丹 谷喜吉 叶玮[1] 李凤全[1] 

机构地区：[1]浙江师范大学地理过程实验室,浙江金华321004

出　　处：《浙江师范大学学报（自然科学版）》2014年第1期108-114,共7页Journal of Zhejiang Normal University:Natural Sciences

基　　金：国家自然科学基金资助项目(41371206)

摘　　要：采石与地理环境之间的互动是区域人地关系的重要组成部分.根据浙江省现代采石场、古采石场遗址调查数据,结合浙江省地质、交通、水系、古气候变化及历史地理背景,探讨了浙江省隋唐宋时期采石格局及其驱动因素.研究表明:隋唐宋三朝,浙江古采石遗址数量增加明显,为历史时期采石活动的鼎盛期;期间杭州湾沿岸、浙东沿海、钱塘江流域三大采石中心相继出现并发展,是历史采石格局由分散→单一中心→多中心演化的重要时期.隋唐宋时期采石格局的形成和采石业的发展受该时期凿建运河、围堰建闸、兴筑海塘、建设港口、修建都城等工程建设和岩性、水系、古气候变化等自然环境因子的共同驱动.Quarrying and its environmental effects revealed important regional human-earth relationship. Based on the investigation of quarry relics and modem quarries in Zhejiang province, combining the geology, trans- portation, river systems, paleoclimate changes and historical geography background, the quarrying patterns and their environmental drivers in Zhejiang province during Sui, Tang and Song dynasties were discussed. The results showed that the number of quarry relics increased obviously in that period, which were the heyday of quarrying during historical periods; The quarrying appeared and concentrated in Hangzhou Bay area, East Zhejiang coastal area and Qiantang river basin; The quarrying patterns underwent scattered-monocentric-poly- centric distribution evolution. The development of quarrying and the forming of quarrying patterns were driven by the projects of canals, weirs, dams, seawalls, ports and capital city construction and environmental factors including water systems, lithology and paleoclimate changes.

关 键 词：隋唐宋时期 采石格局 环境驱动 岩性 古气候 

分 类 号：K925[历史地理—人文地理学]