A Preliminary Study of Formation Mechanism of Tectonic Landform of Fujian

  • 福建构造地貌发育机制初探
  • 来源:互联网摘选更新时间:2026-07-01 19:12:02

  • 重点词汇
  • ofprep. 关于;属于…的;由…制成;
  • studyn. 学习;研究;功课;课业;学业;用于某些学科名称;书房;
  • aart. 一(个);每一(个);任一(个),用于辅音音素开头的单词前
  • mechanismn.[生]机制,机能,[乐]机理;(机械)结构,机械装置[作用],(故事的)结构;[艺]手法,技巧,途径;机械作用;
  • formationn.形成;构成,结构;形成物;编队,队形;奇峰,怪石,某种形状的云;
  • landformn.地形;
  • fujian福建(位于中国东部沿海);
  • tectonicadj.地壳构造的
  • 相关例句
1、

The causation of the generation of this phenomenon is studied with tectonic landform feature and climatic hydrologic condition.

并根据新疆构造地貌特点和气候水文条件,对这一现象的产生作了初步探讨。

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2、

Tectonic landform in the south of the South China Sea

南海南部海域构造地貌

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3、

Third, space effect on the current tectonic activity is extruded from the thermal radiation field of land surface by the difference between influence of atmosphere and tectonic activity on land surface.

再次,根据构造因素与非构造因素对地表热辐射影响的空间差异提出均值梯度法,突出构造活动信息;

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4、
5、

The lake in this basin was formed before the volcanic eruption. Thus, it is not a checked-np lake, but a tectonic lake in genesis.

盆地中湖泊的形成是在火山喷发之前,不是壅塞成因而是构造成因。

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6、

Types of lakes: tectonic lake, crater lake, fluvial lake, dammed lake, glacier lake, karst lake, Aeolian lake, impact crater lake and artificial lake.

湖泊分类:构造湖、火山口湖、冲积残留湖、堰塞湖、冰川湖、喀斯特湖、风成湖、陨石撞击湖和人工湖。

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7、

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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8、

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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10、

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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11、

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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12、

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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13、

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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14、

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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15、

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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16、

Tectonic stress fields control all levels of events during the evolution of tectonic geology and this kind of function acts through the geological process.

构造应力场控制了构造地质演化中的各级事件,并贯穿于整个地质演化中。

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17、

Hence the terrain along this railway is complicated and rugged. Along with the influences of repeated tectonic movements, the geology is very complex, resulting in various hazardous geologic phenomena such as rock fall, landslide and debris flow.

沿线地形复杂,地势险峻,而且由于历次构造运动的强烈影响,地质情况非常复杂,致使沿线大部分地区存在崩塌落石、滑坡、泥石流等各种不良地质现象,被称作地质博物馆。

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18、

The tectonic evolution and petroleum geology are characterized by that ① Laiyang period is dextral pull-apart rifting stage mainly formed source rocks;

胶莱盆地构造演化及油气地质特征是:莱阳组沉积期为右行走滑拉分裂谷阶段,是主要的生油岩形成期;

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19、

Tectonic Evolution and Petroleum Geology Characteristics of Petroliferous Salt Basins Area Along Passive Continental Margin, West Africa

西非被动大陆边缘含油气盐盆地构造背景及油气地质特征分析

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