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1)  Hanzhong and Ankang basin
汉中与安康盆地
1.
Characteristics of seismicity in Hanzhong and Ankang basin;
汉中与安康盆地地震活动特征
2)  Hanzhong basin
汉中盆地
1.
In this paper,a new model for evaluating the regional water resources development and utilization is built up based on set pair analysis,and the model is applied in evaluation of water resources development and utilization in Hanzhong basin.
基于集对分析方法建立了区域水资源开发利用程度的评价模型,并应用该模型对汉中盆地水资源的开发利用程度进行了综合评价。
2.
In this paper,a general model of regional water resources development and utilization is established and the stage of water resources development in the plain area of Hanzhong Basin is determined by fuzzy overall appraisal model.
本文提出了区域水资源开发利用的总体模式,通过阈限分析,利用模糊综合评判模型确定了当前汉中盆地平坝区水资源开发利用所处的阶段,并提出相应的开发对
3)  Hanjiang Ankang
汉江安康
4)  Beikang basin
北康盆地
1.
Based on the analyses of multi_channel seismic data more than 20,000 kilometers in Beikang basin, the origin type and evolution history of the basin are discussed.
通过对北康盆地 2 0 0 0 0余千米多道地震资料的分析 ,探讨了该盆地的成因类型和形成演化史。
2.
Located in mid Nansha waters, the Beikang basin is a Cenozoic sedimentary basin where Cenozoic sedimentary cover rock is extensively developed.
北康盆地是位于南沙中部海域的新生代沉积盆地 ,新生代沉积盖层在盆地内广泛发育 ,根据地震反射特征及地震反射界面的区域对比 ,盆地盖层可进一步划分为 3个构造层。
5)  Yongkang basin
永康盆地
1.
Analysis of sedimentation and genetic stratigraphic framework of Yongkang basin in Zhejiang province;
浙江永康盆地沉积作用与成因地层格架分析
6)  Mangkang basin
芒康盆地
1.
Elemental and Pb-Sr-Nd isotopic geochemistry tracing indicates that the high-K volcanic rocks of the Lawuxiang Formation in the Mangkang basin were derived from an EMII enriched mantle in continental subduction caused by transpression.
元素和Pb-Sr-Nd同位素地球化学示踪结果表明,西藏芒康盆地内拉屋乡组高钾火山岩是在转换压缩引起的陆内俯冲背景下产生的,其可能源区为EMII型富集地幔端元。
2.
The author has taken the high-K magmatic rocks in the Nangqian and Mangkang basins at the northern segment of the JRRSZ as examples to date their 40Ar/39Ar ages and determine their genetic mechanism via elemental and isotopic tracing.
作者以该构造带北段的囊谦和芒康盆地高钾岩石为研究对象,通过~(40)Ar/~(39)Ar定年和配套的元素-同位素地球化学示踪研究,确定了该构造带北段高钾岩浆活动的时限,并探讨了高钾岩石的成因机制。
补充资料:樊二十三寺御赴汉中判官
【诗文】:
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幕府辍谏官,朝廷无此例。至尊方旰食,仗尔布嘉惠。
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陶唐歌遗民,后汉更列帝。恨无匡复姿,聊欲从此逝。



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【出处】:
全唐诗:卷217_8
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