1) Zhiyun area
紫云地区
2) Ziyang area
紫阳地区
1.
[Method] The new method of flame atomic absorption spectrometry(FAAS) for determining Se content in Se-enriched tea in Ziyang area of Ankang city was established.
直接添加100 ml混酸HNO3-HClO4作为分解剂,湿法硝化分解安康市紫阳地区富硒茶叶效果显著。
3) Yunnan area
云南地区
1.
Precursor anomaly feature of dynamic pattern of groundwater level in Yunnan area;
云南地区水位动态图像的前兆异常特征
2.
Study on synthetical anomaly characteristics of short-term precursors of strong earthquakes in Yunnan area;
云南地区强震前兆短期综合异常特征研究
3.
Then we calculated the VP/VS ratio of the Yunnan area and analyzed its regional distribution characteristics.
从1998~2006年间云南地区数字地震台网记录中,选用有4个以上台记录到的震相清晰的直达Pg波、Sg波的到时(包含Pg、Sg的到时差在20~25 s的远台和小于0。
4) Yunkai area
云开地区
1.
An integrated study of geological structural characteristics, granite petrology and time_space distribution regularity of deposits indicates that the Mesozoic lithosphere of Yunkai area experienced three tectonic evolution phases: the collision between 201 and 277 Ma, the tectonic transformation from compression to extension between 154 and 160 Ma, and the extension between 80 and 100 Ma.
文章通过对云开地区地质构造、矿床时空分布以及中生代花岗岩类岩石的岩石学及地球化学特征的综合研究,认为区内中生代岩石圈构造经历了二叠—三叠纪之间的碰撞挤压、侏罗纪的构造转换及白垩纪的拉张伸展 3个阶段的演化过程,大规模成矿作用受控于燕山早期岩石圈的构造转换及燕山晚期的拉张伸展的岩石圈动力学背
2.
The Sedimentary chert formation (Sinian D fromation) at the top of the Precambrian in Yunkai area,western Guangdong and southeastern Guangxi displays banded,lamellated,massive and pseudobrecciated structures.
地处粤西和桂东南的云开地区前寒武系顶部的硅岩沉积建造(“震旦系D 组”),具有层状、纹理状、块状和假角砾状构造。
3.
It is the age of the isobaric cooling event of static recrystallized carbonate minerals in marble post deformation, reflecting approximately the age of metamorphism and deformation after the hydrothermal deposition in late Neo Proterozoic in the Yunkai area.
结合野外和岩相学研究结果,大理岩的Pb同位素记录了大理岩碳酸盐矿物后变形静态重结晶之后等压冷却事件,(555±68)Ma大致反映了云开地区新元古代末期热水沉积事件之后的一次变质变形事件的年龄,从而确立了新元古代末期热构造事件的存在,这对揭示云开地区前寒武纪地质演化历史具有十分重要的意义。
5) Yunnan
[英][ju:'nɑ:n] [美][ju'nɑn]
云南地区
1.
The Spatial-temporal Characteristics of Continuous Occurrence of Mid-strong Earthquakes and Its Modulation Ratio in Yunnan Area;
云南地区中强地震连发及其调制比的时空展布特征
2.
The spatial and temporal distribution of focal depth before strong shocks in Yunnan;
云南地区强震前震源深度的时空展布
3.
Analysis of the Characteristics of Source Precursor and Field Precursor of Groundwater in Yunnan;
云南地区地下水动态的地震源兆与场兆特征分析
6) Yunnan region
云南地区
1.
Study on velocity ratio(V_p/V_s) anomaly of earthquake sequences in Yunnan region;
云南地区地震序列的波速比(V_P/V_S)异常研究
2.
Analysis of teleseimically trigged seismicity in Yunnan region under influence of the Indonesia large earthquakes with M8.7 and M8.5;
印尼8.7、8.5级巨震对云南地区地震活动的远震触发分析
3.
The Characteristics of Short-term and Impending Seismic Anoma ly before Strong Earthquakes in Yunnan Region;
云南地区强震前地震活动的短临异常特征
补充资料:北京紫云山
紫云山位于怀柔县北21公里,是一处景色秀丽多姿的风景区。紫云山方圆3000亩融黄山之奇,华山之险,峨眉之秀于一体,通天河如丝带般串起88个碧潭。景区内有镇守翠谷的武士、巍峨挺拔的擎天石、洁白如玉的莲花峰、怪石上的济公、千年厮守的企鹅夫妻、威武的下山虎,还有飞来石、紫云池、神女池等,惟妙惟肖,栩栩如生来此能真正体会到大自然的神奇。
交通线路: 东直门乘936或宣武门乘游17路直达;或乘916路到怀柔站,换乘中巴前往
景点门票: 16元、学生8元
景点位置: 北京市怀柔县怀北镇北部云蒙山西麓
说明:补充资料仅用于学习参考,请勿用于其它任何用途。