1) Ba Yan Hot
巴彦浩特
1.
The research on Urban ecological environment planning in arid area was developed,taking the Ba Yan Hot of eastern edge of Teng Ge Li desert as an example.
生态环境规划与建设是干旱区城市实现区域与城市可持续发展的重要保证,本文以位于腾格里沙漠东部边缘的巴彦浩特为例进行干旱区城市生态环境规划研究。
2) Bayehot
巴彦浩特镇
1.
On base of analysis on the characteristics of urban land classification and evaluation in Bayehot, the evaluating characteristics of base land value in Bayehot were summerized, the average of classification base land value,the average of grade base land value ,the similar chain indexes of land value and similar rate indexes of land value at all levels were calculated.
本文在分析巴彦浩特镇土地定级估价的基本特点的基础上,根据历年基准地价的测算数值,测算并分析级别平均地价、分类平均地价、同类各级地价环比指数、同类各级地价比率指数,为了更能达到直观的效果,把这些数值绘制成表格并且做成图形,总结出比率变动的共同特征和随时间变化的动态特征。
3) the Bayanhaote Basin
巴彦浩特盆地
1.
In the Bayanhaote Basin,there is a linear correlation between the depths of the enclosure samples in different ages and the homogenization temperatures of enclosure, especially those in middle and later periods, and there can be divided in vertical direction into four stages which are immature stage,low mature stage, mature stage and high mature stage.
通过巴彦浩特盆地石炭系流体包裹体的研究认为 ,不同时代的样品尤其是中晚期包裹体的均一温度与埋藏深度之间存在良好的线性关系。
2.
According to exploring result in the Bayanhaote Basin,the petroleum system is analyzed, and two petroleum systems are distinguished,those are Hercynian Indosinian de.
根据巴彦浩特盆地现有的勘探成果 ,对盆地含油气系统进行了分析 ,识别出盆地南部海西期—印支期石炭系破坏型含油气系统和北部燕山期—喜山期石炭系再生型含油气系统 ;在此基础上通过对油气勘探有利区带的分析 ,指出盆地北部及其中的黑汕托—赛勒背斜构造带是盆地开展油气勘探的有利区
4) Bayanhot Basin
巴彦浩特盆地
1.
Carboniferous Reservoir Features and Diagenesis,Bayanhot Basin;
巴彦浩特盆地石炭系储层特征及成岩作用
2.
The structural evolution of Bayanhot Basin underwent a structural transform from compressional deformation to extensional deformation.
巴彦浩特盆地的构造演化经历了由早期的挤压变形向晚期的伸展变形的构造转换 ,因此 ,盆地内发育有多种构造类型 ,从断裂的性质看 ,既有正断层 ,又有逆断层和走滑断层 ;从构造的组合型式上看 ,既有挤压型构造组合 ,又有伸展型构造组合 ,其中挤压型构造组合包括叠瓦状逆冲断层组合、滚板构造、冲起构造和铲形逆断层与牵引背斜、牵引向斜组合 ;伸展型构造组合包括铲形正断层与反向断层、滚动背斜组合及地垒和地堑组合两种型式。
5) Bayanhaote basin
巴彦浩特盆地
1.
Based on age study of apatite fission track of Carbonif-erous in Bayanhaote basin,it is believed that the annealing age was after Jurassic and Jurassic had not experienced tem-peratures over120℃ever since then while Carboniferous largely reached the highest annealing temperature of apatite at the end of Cretaceous.
巴彦浩特盆地石炭系磷灰石裂变径迹年龄研究分析认为,该盆地磷灰石裂变径迹退火年龄自侏罗纪以后,侏罗系再未经历高于120℃的温度,而石炭系在白垩纪末普遍达到磷灰石的最大退火温度。
2.
The surface of Bayanhaote basin is covered largely by desert and gobi.
巴彦浩特盆地地表大部分被沙漠和戈壁覆盖。
6) Shenzhen-Bayanhaote
深圳-巴彦浩特
补充资料:浩特
蒙古族牧人居住的自然村,也指城市。[蒙]
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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