1) Zabuye Lake area
扎布耶湖区
1.
This paper introduces the characteristics of sediments and their contained 6 genera and 20 species of ostracods and 2 genera and 3 species of charophytes revealed by nearly 84 m deep well SZK02 drilled in the Zabuye Lake area,Tibet.
本文主要根据西藏扎布耶湖区SZK02孔所揭露的近84m剖面的沉积物特征与其产的介形类6属20种,轮藻类2属3种,结合14C、ESR、U-series地层测年等,初步认为该区128～1。
2) Zhabuye salt lake
扎布耶盐湖
1.
The Preliminary Study on the Equilibrium Solubility and Crystallization Laws of Lithium Carbonate Based on the Composition of Zhabuye Salt Lake Brine
扎布耶盐湖卤水碳酸锂恒温平衡浓度和结晶规律初步研究
2.
This paper presents the experimental data of metastable phase equilibrium of Li~+/Cl~-,CO_3~(2-),B_4O_7~(2-)-H_2O quaternary system at 298 K for Zhabuye salt lake in Tibet,from which the metastable phase diagram and physicochechemical properties(density,pH value,conductivity and refractive index) vs composition diagram is drawn.
根据对西藏扎布耶盐湖四元子体系L i+/C l-,CO32-,B4O72--H2O 298 K介稳平衡实验数据,绘制出的介稳平衡相图及物化性质(密度、pH值、电导率、折光率)组成图的研究结果表明:该四元体系属简单共饱型,无复盐或固溶体形成;其溶解度等温图含有一个共饱点、3条单变量曲线和3个结晶相区;3个结晶相区分别对应为L i2B4O7。
3) Zabuye Salt Lake
扎布耶盐湖
1.
Study on the Crystallization Law of Salts form the Brine after Freezing through the Normal Temperature(20℃)Evaporation in Zabuye Salt Lake;
扎布耶盐湖冷冻后卤水常温蒸发(20℃)析盐规律
2.
25℃-Isothermal Evaporation of Autumn Brines from the Zabuye Salt Lake,Tibet,China;
西藏扎布耶盐湖秋季卤水25℃等温蒸发研究
3.
Sedimentary Characteristics and Paleoenvironmental Records of Zabuye Salt Lake,Tibetan Plateau,since 128 ka BP;
西藏高原扎布耶盐湖128ka以来沉积特征与古环境记录
4) Zabuye saline lake
扎布耶盐湖
1.
Zabuye saline lake, situated in the hinterland of Tibet plateau, is a contemparysaline lake deposit.
扎布耶盐湖位于青藏高原腹地，是一个现代盐湖矿床。
2.
The natural geography condition of Zabuye saline lake which is located in Qinghai-Tibet plateau is very special.
青藏高原的扎布耶盐湖自然地理条件特殊，新生代以来，经历了快速的演变过程，现今已成为强烈萎缩的盐湖。
5) Zhabuye type saline lake
扎布耶型盐湖
补充资料：埃布里耶潟湖
在科特迪瓦南部几内亚湾北岸，是阿比让港区所在地。东西长112公里，面积550平方公里，平均水深7-8米。有长3.2公里、宽370米、深15米的弗里迪运河通几内亚湾，海轮由此进出阿比让港。东、西端也各有运河通相邻潟湖，使周围地区所产木材、锰矿石可经阿比让港输出。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条