| 浅析四川通江诺水河地质公园岩溶景观成因 |
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| 引用本文： | 曹俊,杨俊义,郭建强,杨更.浅析四川通江诺水河地质公园岩溶景观成因[J].四川地质学报,2009,29(2):224-227. |
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| 作者姓名： | 曹俊 杨俊义 郭建强 杨更 |
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| 作者单位： | 四川省地质矿产勘查开发局区域地质调查队,成都,610213 |
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| 摘 要： | 诺水河地质公园内完整保留了岩溶作用各阶段的地质现象，形成了主题突出、类型多样的地质遗迹景观组合。该区出露了厚达2248m的石灰岩地层，为岩溶作用提供了丰富的物质基础。自0．65亿年的古近纪以来受推覆构造影响，使区内地壳呈阶段式上升，产生大量水平裂隙和纵张裂隙，为岩溶作用提供了良好的通道。岩溶洞内形态万千、绚丽多彩的钙华景观则是含Ca^2＋的水流经滴水作用、面状流水作用、池水作用、协同水作用、毛细管和旋卷流水作用的杰作。
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| 关 键 词： | 岩溶景观 米仓山台穹 通江诺水河 |
A Brief Talk on Genesis of Karst Landscape in the Nuoshuihe Geopark, Tongjiang, Sichuan |
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| CAO Jun,YANG Jun-yi,GUO Jian-qiang,YANG Geng.A Brief Talk on Genesis of Karst Landscape in the Nuoshuihe Geopark, Tongjiang, Sichuan[J].Acta Geologica Sichuan,2009,29(2):224-227. |
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| Authors: | CAO Jun YANG Jun-yi GUO Jian-qiang YANG Geng |
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| Institution: | Regional Geological Surveying Team;BGEEMRSP;Chengdu 610213 |
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| Abstract: | There are all the karst landscapes in the Nuoshuihe Geopak which form many and varied geoheritage landscape associations.Limestone with a thickness of 2248 m is exposed in this region which lays material foundation for karstification.Since the Paleogene(65 Ma),napping has resulted in step-type cymatogeny and a great deal of horizontal and vertical fissures which provide good channel for karstification.The travertine landscape in karst caves should be attributed to Ca+2-rich running water action. |
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| Keywords: | karst landscape Ca+2-rich running water Micangshan anteclise Nuoshui River Tongjiang |
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