摘要
渝东地区的自然盐泉是因地质构造与地貌特征的巧合使三叠系中部的含盐层上升到山上的特殊地理环境而形成的。渝东地区的人工盐井都是由自然盐泉演变而来的，推动自然盐泉向人工井演进的动力是洪水。这就是说，渝东地区的人工盐井是先民们与洪水长期搏斗的结果。
The natural salt spring in the region of Eastern Chongging was formed by the special geological environment that the coincidence of structure and surface characteristic made the central salt layer of Triassic go up to the mountains. The artificial wells in the place were changed from natural spring.The motive of the evolution was flood.That is to say that the artificial wells in the place was the result of the ancestors longly fighting with flood.
出处
《盐业史研究》
2002年第1期32-40,共9页
Salt Industry History Research
