长江流域资源与环境 >> 2016, Vol. 25 >> Issue (07): 1135-1141.doi: 10.11870/cjlyzyyhj201607016
龚继文1,2, 李崇明1,2, 程艳茹2, 张韵2, 赵丽2
GONG Ji-wen1,2, LI Chong-ming1,2, CHENG Yan-ru2, ZHANG Yun2, ZHAO Li2
摘要: 本文基于GMS平台,在综合分析重庆某山区地质平面图、地质剖面图、钻孔资料等数据基础上构建了三维可视化地质模型。模拟结果表明:研究区砂泥岩倾斜互层的沉积顺序和不同岩性的空间分布情况与该区已有资料相一致;模型剖面与实际地质剖面面积之比约为1.15,主要岩性面积百分比相对误差绝对值均在15%以内。运用该模型概化为三维水文地质模型,模拟得出研究区地下水流场空间分布,体现了三维地质模型在地下水数值模拟方面的运用价值。该模型的构建为山区区域地质结构研究提供了参考,也为今后该地区开展地下水相关工作打下了基础。
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