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geological相关的网络例句

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与 geological 相关的网络例句 [注:此内容来源于网络,仅供参考]

The relatively rapid complexification in most recent geological history suggests to Brooks "that problem solving behavior, language, expert knowledge and reason, are all pretty simple once the essence of being and reacting are available."

在地质学史上,复杂性在近代有了较快的发展。这使布鲁克斯想到:一旦具备了生命和对外界做出反应的基本条件,就可以轻而易举地演化出解决问题、创造语言、发展专业知识和进行推理等高级智能。

According to the geological features and the grade data of ore-forming elements,which are analysed systematically by using Yang Chizong filter method,in several deposits of Hu-Bi-type copper deposit,we propose that such orefield is controlled compositely by folds-thrust faults of NE direction and faults of NW direction,and that ore pillars are formed in the intersection area of structures mentioned above.

应用杨赤中滤波法系统分析了胡篦型铜矿几个矿床成矿元素的品位资料,结合矿床地质特征研究,认为该类矿床不仅受NE向褶皱冲断构造控制,而且还受NW向断裂构造复合控制,在其交汇部位形成矿柱。

On basis of analysis of geological characteristics of compressional basins in the world,the concept and theory of piedmont and piedmont hydrocarbon accumulation was proposed.

在分析了国内外压性盆地油气地质规律的基础上,提出了&山前&和&山前油气富集成藏&的概念及理论认识。

As the basic condition of human's surviving and developing, the geological ecology environment is the foundation of continuable development of society and economy.

地质生态环境是人类生存和发展的基本条件,是社会和经济可持续发展的基础。

The structural features of the Cenozoic contractional deformation in the transition belt between Kuche depression and southern Tianshan uplift have been revealed by geological outcrop, seismic data, welllog and CEMP(Continuous Electromagnetic Profile)data; it is found that these features are difficult to be interpreted by the typical "Atype" subduction model. This article advances a "nonsubduction" contractional deformation model, i.e., the "delaminating contraction and vertically stacking" model.

用地面露头、地震和CEMP勘探资料揭示的库车坳陷-南天山盆山过渡带构造变形特征难以用经典的&A型俯冲&冲断褶皱楔变形模型来解释,因而文中提出一种&分层变形、垂向叠置&的&非俯冲&收缩构造解释模型。

And some test indices obtained from different geological units in Beijing area are selected and studied contrastively.

研究目的:确保高质量地搜集北京地区锤击取芯钻进和回转钻进工法土样的试验成果数据,分析不同工法试验指标的关系,针对北京段的地层条件,给选择可靠的备选钻探方法提供技术依据。

Based on the settings and geological and geochemical characteristics of granitoids of different orogenic belts (exemplified by orogenic granitoids in Altay, East Kunlun, Yanshan in North China, Northeast China and Nanling in South China), the relationships between granitoids and continental crustal growth are discussed, and five modes of continental crustal growth in the continent of China are proposed;they are as follows:(1)the Altay mode of continental growth is that the material and heat of the Paleozoic convertive mantle formed on the background of the Paleo-Asian Ocean were input into the Paleozoic continent and mixed with the materials of the upper crust;(2) the East Kunlun mode is that the basement of the Proterozoic orogenic belt was reworked by the heat input and materials of the Paleozoic-early Mesozoic convective mantle formed on the background of TTG continental crust of the Proterozoic orogenic belt;(3) the Northeast China style is that the Phanerozoic continental crust was reworked by the heat input and materials from the convective mantle formed on the background of the Yanshanian Central Asian orogenic belt;(4) the Yanshan mode is that the Archean basement was reworked by the heat input and materials from the Yanshanian convective mantle;and (5) the Nanling mode is that in South China what was input by the Yanshanian convective mantle into the continent was mainly heat and subordinately materials and the crustal material recycle was the dominant mode for the continental growth (showing zero continental growth).

根据不同造山带花岗岩的形成背景,地质地球化学特征差异,以阿尔泰,东昆仑,华北燕山,东北和南岭造山带花岗岩为例讨论花岗岩与大陆地壳生长的关系,区分出中国大陆的5种大陆地壳生长方式:阿尔泰式是古亚洲洋背景上形成的古生代对流地幔物质,热输入和上地壳混合为主的方式;东昆仑式是元古代造山带TTG陆壳背景基础上古生代—早中生代对流地幔物质和热输入,改造元古宙造山带基底的方式;东北式是燕山期中亚造山带背景上对流地幔物质和热输入改造显生宙陆壳的生长方式;燕山式是燕山期对流地幔物质和热输入改造太古宙基底的方式;南岭式燕山期对流地幔输入大陆的是以热为主,物质为辅,大陆地壳生长是以陆壳物质再循环为主的生长方式。

In this study, we take 1999 Mw7.6 Chi-Chi earthquake for example to study the effect of sub-fault model and layered geological crust model to the coseismic deformation.

本文以1999年Mw7.6级集集地震为例,讨论不同的位错模型和介质模型(均匀、层状均匀及横向不均匀等)对同震形变的影响。

However, when cosmogenic nuclidesare used, as more information as possible about the geological process of the research area should be used inord er to explain the result as reasonable as possible.

只是应该注意,进行这类工作时首先要对研究地区的地质过程有清楚了解,并尽可能与相关资料进行对比,以期对结果给予合理的解释。

Ca is widely abundant in nature and its rodioisotope 41 Ca is a cosmogenic nuclide with a half\|life of 10 5 years. However, the 41 Ca/ 40 Ca ratio in natural samples is very low and can only be measure d by accelerator mass spectrometry. The application of 41 Ca is ve ry i mportant not only in the life science but also in geological dating, global envi ronment change studies and astrophysics.

1 引言Ca在自然界中广泛存在,它不仅是人体中含量最丰富的元素之一[1] ,也是众多其他物质的组成部分。41Ca(半衰期为 1.0 3× 10 5a)属于Ca的放射性同位素中的一种,其衰变方式为轨道电子俘获,只发射3.3keV的X射线,天然样品中41Ca 40 Ca的值很小。

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