1) Linfen-Yuncheng basin
临汾-运城盆地
1.
Fluorine content in soils of the Linfen-Yuncheng basin,southern Shanxi,China,and its influence factors;
晋南临汾-运城盆地土壤氟含量及其影响因素
2.
Change of the arsenic content in soils of the Linfen-Yuncheng basin,Shanxi,China;
山西临汾-运城盆地土壤中As含量的变化规律
2) Linfen Basin
临汾盆地
1.
The Evolution and its Contributing Factors of Linfen Basin Since Middle Quaternary;
临汾盆地中更新世中晚期以来的演化历史及成因分析
2.
The Evolution of Pedogenesis Environment and Influence of Human Activities in Linfen Basin During the Holocene;
临汾盆地全新世成壤环境演变及人类活动影响
3.
Linfen Basin is an important basin in the central part of Shanxi province.
通过对临汾盆地王绪及其邻近地区黄土地层中所含抱子花粉、右脊椎动物化石、颗粒成分、磁化率、古土壤、结构构造以及接触关系等综合研究，将王绪剖面上的黄土划分为下更新统、中更新统及上更新统三层，并同洛川、午城两地区的午城黄土、离石黄土及马兰黄土地层对比。
3) Linfen faulted basin
临汾断陷盆地
1.
Dongkang mineral water is Located at the edge of Linfen faulted basins.
东亢矿泉水处于临汾断陷盆地边缘山前地带。
4) Yuncheng Basin
运城盆地
1.
Holocene Environment Change of Pedogenesis and Erosion phases on Pluvial-alluvial Fan in Yuncheng Basin,Shanxi Province;
运城盆地洪积平原全新世环境演变与侵蚀阶段研究
2.
Distribution and causes of formation of high-fluorine groundwater in Yuncheng basin;
浅谈运城盆地高氟地下水的分布及成因
5) Fenwei basin
汾渭盆地
1.
The Holocene Paleoflood and Sheet Erosion-deposit Events in the Fenwei Basin;
汾渭盆地全新世古洪水和侵蚀沉积事件研究
2.
The Environmental Changes and the Land Desertification of Fenwei Basin over the Past 1.2Ma;
汾渭盆地1.2Ma以来的环境变化与沙漠化过程
3.
In 1970's, it is found that natural gas evidence in Neogene-Paleogene period stratum, such as helium, methane and nitrogen, etc, when they had explored oil in Fenwei basin.
20世纪70年代,前人在汾渭盆地进行石油勘探时,于新近—古近系钻遇氦、甲烷、氮等天然气,由于当时以新生界石油勘探为目的,所以未能开展进一步工作。
6) Fen-Wei basin
汾渭盆地
1.
The Fen-Wei basin is the most serious area of the ground fissure formation in China.
汾渭盆地是我国地裂缝发育最强烈的地区,地裂缝类型多样,成因复杂。
补充资料：金运临酉
金运临酉
金运临酉 运气术语。指乙酉岁会。乙为金运，酉为金的正位，中运金与岁支酉同气。《素问·六元正纪大论》：“金运临酉……所谓岁会，气之平也。”新校正云：“金运临酉，乙酉岁也。”
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