tectonic geomorphology

The evolution of the modern tectonic geomorphology in Lianyungang, the upright distributing of the sea erosion geomorphology at Yuntai mountain area, and change of the coastline reflect neotectonic movements intension, direction and the course of development in parts of an area.

连云港现代构造地貌的发育、海蚀地貌在云台山区的垂直分布，以及海岸线的位置变动，反映出新构造运动在局部地区的运动强度、方向和发展过程。

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Analysis of the data about strata, tectonic geomorphology and fault activity indicate that newest activity of the south of Nujiang fault is early-middle Pleistocene, namely, there is no obvious signs of activity since late Quaternary.

综合地层、构造地貌和断层活动的资料认为怒江断裂带南段在早-中更新世有过活动，而晚第四纪以来没有明显的活动迹象。

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The tectonic analysis system of geometry analysis, kinetics analysis, and dynamics analysis are put forward, which is of universal significance to the study of tectonic geomorphology.

总结、提出了对构造地貌研究具有普遍意义的几何分析、运动分析和动力分析的构造地貌分析体系；

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Based on analysis of relative documents, the characters, contents, research methods of this learning branch are presented, and its research progress in China is reviewed and summarized in this paper. Finally, the future research direction of tectonic geomorphology is discussed.

本文在分析相关文献的基础上，论述了构造地貌学的特点、研究内容、研究方法，回顾了在中国的研究进展，最后提出了构造地貌学今后的研究动向。

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The strong neo-tectonic movement and special tectonic setting produced specific Yellow River and typical landscape of tectonic geomorphology in the area.

强烈的新构造运动和特殊的构造位置，造就了本区特殊而典型的构造地貌景观。

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The study to tectonic landform is an analysis using integrated methods of geomorphology structural geology.

构造地貌是指由新构造运动直接形成的一种动态的、积极活跃的地貌类型.

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Based on the point of tectonic geomorphology, the geomorphology in and outside the Taiyuan Basin were divided into four geomorphologic units: periphery block rising mountain, slightly rising hill tableland, pluvial sedimentation plain, and alluvial sedimentation plain.

应用构造地貌的观点，把太原盆地及其边缘地貌分为：外围断块抬升山地、抬升轻微的丘陵台地、山前堆积的洪积倾斜平原和沉降堆积的冲积平原4种地貌单元。

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Its tectonic geomorphology is characterized by clear linear fault scarps, the average vertical slip rate of the fault is about 0.41 ± 0.27 mm/ a since late period of the late Pleistocene.

断裂在地貌上表现为明显的挤压逆冲断层陡坎，晚更新世晚期以来的平均垂直滑动速率为0.41±0.27mm/a。

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The authors summarize current applications and research methods in several specific Earth science areas, including glacial chronology and geomorphology, tectonic geomorphology, site-specific weathering, erosion and regolith/ soil production, watershed and sediment transported processes, alluvial, and fluvial and beach landforms.

简述其在冰川地貌、构造地貌、岩石风化、侵蚀与风化壳（土壤）形成、流域侵蚀与搬运过程、阶地、台地以及喀斯特地貌等方面的研究现状。

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According to many researchers achievement , the response of fluvial geomorphology to tectonic movement is discussed.

以前人的研究工作为例, 讨论了河流地貌对构造活动的响应.

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On the Evolutional Model of the Tectonic Geomorphology of the Okinawa Trough

冲绳海槽构造地貌发育模式研究

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The method of tectonic geomorphology was used to study tectonic activity and geomorphological features of Su-Lu segment in late Quaternary.

应用构造地貌学方法分析了断裂带晚第四纪构造活动及地貌特征；

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Analysis of the filling sequence indicates there may be four tectonic activity periods after formation of the basin, which are proved in fault activity and tectonic geomorphology.

而对充填序列的分析得出盆地形成以来可能存在四个构造活跃期，并从构造地貌和断层活动方面进行论证。

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