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在黄河的形成与演化研究中，长久被轻视但极为重要的记录是河道的形态、产出位置及其与河岸地质体的依存关系。研究认为，黄河河道总体呈现长线型延伸、短折线拐弯、锯齿状摆动3种延伸样式，区域大地构造演化、断裂构造作用等内动力地质作用是黄河河道形成与演化的主控因素，青藏高原、鄂尔多斯地块周缘和华北平原是区域大地构造演化所形成的3个独特构造-地貌单元，流域的构造因素分别造就了反Z形、“几”字形和宽V形3种几何学形态迥异的河道组合样式，3种样式河段在形成与演化中，衍生出各自特有的地质、工程、开发与保护等方面问题，据此提出了开发治理建议。
Abstract：In the formation and evolution of the Yellow River, long underestimated but extremely important records are the form and location of the river channel, as well as the interdependence between riparian geological bodies. The study shows that the Yellow River channel generally presents three extension styles of long line extension, short bend and zigzag swing. Regional tectonic evolution, faulting tectonism and other internal dynamic geological processes are the main controlling factors for the formation and evolution of the Yellow River channel. The Qinghai-Tibet Plateau, the margin of the Ordos block and the North China Plain are three unique tectono-geomorphic units formed by regional tectonic evolution, and the tectonic factors in the basin have respectively created three different geometric patterns of river channel combinations, namely, inverted Z-shaped, Ω-shaped and wide V-shaped. During the formation and evolution of the three types of river channel, their own unique issues in geology, engineering, development and protection are derived, according to which the development and management suggestions are put forward.
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基本信息:
DOI：
中图分类号:TV882.1;P642
引用信息:
[1]彭建兵,李永军,王祚鹏等.黄河河道的主控因素及其衍生地质问题[J].人民黄河,2025,47(01):1-7.
基金信息:
国家自然科学基金资助项目(42041006,41790440,42202022); 陕西省自然科学基础研究计划项目(2024JC-YBQN-0324,2023-JC-YB-240); 中央高校基本科研业务费专项(XJ2024002301); 陕西省“双一流”大学建设专项(黄河流域地质图编制项目)