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   喀斯特演化 的翻译结果: 查询用时:0.262秒
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喀斯特演化
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  “喀斯特演化”译为未确定词的双语例句
     forest evolution and comprehensively research erosion morphology-sedimentationsystem, 2. providing basic data for further research on plateau evolution of Yunnanand effects and time domain of Himalayan movement on this area, and 3. providing reference data for karst environment study.
     (2)定量研究石林喀斯特演化过程,构成溶蚀形态-沉积序?
短句来源
     Guilin karst has a diverse landform types and a very long history,with a unique beautiful landscape.
     桂林喀斯特演化历史漫长,地貌类型多样,具有罕见的地貌景观,是世界罕见自然美的地带;
短句来源
  相似匹配句对
     MODELS OF KARST GEOMORPHOLOGICAL EVOLUTIONS IN CHINA
     中国喀斯特地貌的演化模式
短句来源
     Geomorphic Evolution of the Wulong Karst in Chongqing City
     重庆武隆喀斯特地貌及其演化
短句来源
     THE EVOLUTION, OF MINERALS
     矿物演化
短句来源
     Evolution of stars
     恒星演化
短句来源
     The application of fluid inclusions in hydrogeology has also elucidated to search the ground heat water, to study the Karst hydrochemistry,and to explore the change of hydrology and climate in the near future.
     喀斯特水化学的研究;
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  karst evolution
From our own observations, the general physical and geochemical characteristics of the aquifers are perennial and representative of karst evolution at a given moment.
      
This study demonstrates that several parameters are not definitive, and that they do not provide information about the actual status of the karst evolution of the system.
      


Lunan, where the well-known Stone Forest positioned, is one of the typical areas where plateau karst well developed. Karst evolution of this area reflects features of crustal activities of Himalayan movement in eastern Yunnan province Karstification has resulted in a lot of calcic precipitation, including fluvial tufa, cascade tufa, lacustrine tufa, cave tufa as well as Tertiary carbonate rocks. Based on geological and geographical study, systematic sampling have bee taken on calcic precipitations. Ages determinated...

Lunan, where the well-known Stone Forest positioned, is one of the typical areas where plateau karst well developed. Karst evolution of this area reflects features of crustal activities of Himalayan movement in eastern Yunnan province Karstification has resulted in a lot of calcic precipitation, including fluvial tufa, cascade tufa, lacustrine tufa, cave tufa as well as Tertiary carbonate rocks. Based on geological and geographical study, systematic sampling have bee taken on calcic precipitations. Ages determinated by electron spin resonance (ESR) are respectively: 3.15±0.63 Ma, 1.35±0.2 Ma 962±16 thousand years, 329±23 thousand years, 270±14thousand years, 184±8 thousand years, 142±2 thousand years, 79±4 thousand years, 48±5 thousand years. These data, from which major karst evolution periods of this area can be inferred, are puite coincident with other regional age determinations.Significance of these age measurements are: 1. quantitatively study karst stone.forest evolution and comprehensively research erosion morphology-sedimentationsystem, 2. providing basic data for further research on plateau evolution of Yunnanand effects and time domain of Himalayan movement on this area, and 3. providing reference data for karst environment study.

中国云南路南是高原型喀斯特发育最为典型的区域之一,“石林喀斯特”最为著名。该区域喀斯特演化历史及其特点充分反映了云南东部地区在喜马拉雅运动期地壳活动的特征。石林喀斯特化过程中,形成了众多的钙质淀积物,包括河滩钙华、瀑布钙华、湖滩钙华、洞穴钙华及第三系硫酸盐岩。位于不同海拔高度的石林地貌及其间的洞穴钙华,代表了石林发育的不同阶段和过程:地壳抬升-溶蚀、侵蚀-再抬升、钙华沉积。湖滩钙华和河滩钙华的堆积特征也反映了这段历史。准确地确定钙华形成的年龄,便可详细研究石林地区石林喀斯特的演化历史,定量分析地壳抬升幅度和活动规律。作者在运用地质-地貌分析判别基础上,对钙质淀积物系统取样,采用电子自旋共振法(ESR)测定钙华年龄,分别为:315.063万年、135.020万年、92.2±1.6万年、32.9±2.3—27.0±1.4万年、18.4±0.8万年、14.2士0.2万年、7.9±0.4万年、4.8±0.5万年。据此确定了本区喀斯特演化的主要时期。经与大区域测年研究数据相比较,具有很好的一致性。这批数据的地质意义:(1)ESR测年是研究钙华年代的有效方法;(2)定量研究石林喀斯特演...

中国云南路南是高原型喀斯特发育最为典型的区域之一,“石林喀斯特”最为著名。该区域喀斯特演化历史及其特点充分反映了云南东部地区在喜马拉雅运动期地壳活动的特征。石林喀斯特化过程中,形成了众多的钙质淀积物,包括河滩钙华、瀑布钙华、湖滩钙华、洞穴钙华及第三系硫酸盐岩。位于不同海拔高度的石林地貌及其间的洞穴钙华,代表了石林发育的不同阶段和过程:地壳抬升-溶蚀、侵蚀-再抬升、钙华沉积。湖滩钙华和河滩钙华的堆积特征也反映了这段历史。准确地确定钙华形成的年龄,便可详细研究石林地区石林喀斯特的演化历史,定量分析地壳抬升幅度和活动规律。作者在运用地质-地貌分析判别基础上,对钙质淀积物系统取样,采用电子自旋共振法(ESR)测定钙华年龄,分别为:315.063万年、135.020万年、92.2±1.6万年、32.9±2.3—27.0±1.4万年、18.4±0.8万年、14.2士0.2万年、7.9±0.4万年、4.8±0.5万年。据此确定了本区喀斯特演化的主要时期。经与大区域测年研究数据相比较,具有很好的一致性。这批数据的地质意义:(1)ESR测年是研究钙华年代的有效方法;(2)定量研究石林喀斯特演化过程,构成溶蚀形态-沉积序?

Guilin karst is a typical landscape in the world with peak forest plain and peak clusters depression,a unique landform style,geographical feature and systematic evolution feature of synchronism.Guilin karst has a diverse landform types and a very long history,with a unique beautiful landscape.It provides an example of life evolution in the globe.A large number of paleofauna and cones preserve many information about age-old environment and climate in the cone′s sediment,showing peculiar karst eco-environment...

Guilin karst is a typical landscape in the world with peak forest plain and peak clusters depression,a unique landform style,geographical feature and systematic evolution feature of synchronism.Guilin karst has a diverse landform types and a very long history,with a unique beautiful landscape.It provides an example of life evolution in the globe.A large number of paleofauna and cones preserve many information about age-old environment and climate in the cone′s sediment,showing peculiar karst eco-environment and the function of continuous landforms evolution.Guilin Karst is an extremely valuable nature legacy which can′t be reproduced any more.

桂林喀斯特是世界峰林和峰丛喀斯特景观的典型代表地之一,其代表了地球上一种独特的地貌形态和自然地理特征,具有同时态系统演化的特点;桂林喀斯特演化历史漫长,地貌类型多样,具有罕见的地貌景观,是世界罕见自然美的地带;桂林喀斯特区古生物化石十分丰富,是地球生命演化的重要代表地之一;桂林喀斯特洞穴及其次生沉积物丰富,保留了大量古环境和古气候变化的信息,反映了一种特有的喀斯特生态环境和正在进行的地貌演化作用.桂林喀斯特是极为珍贵的、不可再生的、具世界意义的自然遗产地.

 
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