壳体地貌初论 |
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引用本文: | 游长江.壳体地貌初论[J].大地构造与成矿学,1996,20(2):151-157. |
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作者姓名: | 游长江 |
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摘 要: | 壳体地貌是针对传统地貌学存在的基本问题,吸收和运用历史—因果论大地构造学说的理论观点和方法,将地貌成因因素和过程因素综合起来研究的一种地貌学理论和方法。本文运用成因—过程分析法,将地貌及其发展置于大地构造背景下加以研究,提出了地貌四要素和壳体地貌旋回的概念。并主张将侵蚀地貌过程和沉积地貌过程统一起来研究。
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关 键 词: | 壳体地貌 成因—过程分析法 壳体地貌旋回 |
ON THE CRUSTOBODY GEOMORPHOLOGY |
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Abstract: | Crustobedy geomorphology is a kind of theory and method of geomorphology which studies both the results and histories of landforms,by absorbing the theories and methods of historistic-causationist geotectonics,so as to resolve the traditional geomorphological problems. This article puts forward the concepts of "Four geomorphic factors"and "Crustobody geomorphic cycle" by means of result-historyanalysis, prtting the relieves on the backgrouhds of geotectonics, and advocates that both the erosive and sedimentary processes be studied unitedly. |
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Keywords: | crustobody geomorphology result-history analysis crustobody geomorphic cycle |
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