五通桥黄滷水之富集作用

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地质述略(图一) 此区内之地质构造以老龙坝背斜层为主,其背斜轴大致为西南——东北向,横贯泉水场,新塘沽等地。於鼎锅山及寿保场有两局部穹窿层之构成,前者范畴颇大,於此盐田尤具重大 Geological Description The geological structure in this area is dominated by the Laolongba anticline, with its anticlinal axis roughly in the southwest-northeast direction running across the spring water area and the Xintangu area. Yunding Pot Hill and Shou Bao field have two parts of the composition of the fornix, the former a large area, in this Yantian particularly significant
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