1) high-potassium volcanic rocks
高钾火山岩
2) high-Mg ultrapotassic lavas
高镁富钾火山岩
1.
Geochemistry of late Eocene high-Mg ultrapotassic lavas from western Yunnan, China: Constraints on petrogenesis;
滇西晚始新世高镁富钾火山岩的地球化学特征及其岩石成因机制探讨
2.
Normal, reverse and oscillatory zonings are common in clinopyroxene phenocrysts in the Wozhong late Eocene high-Mg ultrapotassic lavas, western Yunnan province.
滇西莴中晚始新世高镁富钾火山岩中单斜辉石斑晶普遍出现正环带结构、反环带结构或韵律环带结构,少量为具绿色核部的单斜辉石(“绿核辉石”)。
3) high Mg# potassic volcanic rocks
高Mg#钾质火山岩
4) high Mg~# potassic-ultrapotassic volcanic rocks
高Mg~#钾质-超钾质火山岩
5) high-K calc-alkaline series volcanic rocks
高钾钙碱岩系火山岩
1.
The characteristics of radiogenic Sr, Pb and unradiogenic Nd show that the Cenozoic high-K calc-alkaline series volcanic rocks from Zuerkengwula mountain area in Northern Tibetan Plateau have a relatively high value of ~(87)Sr/~(86)Sr, a relatively low value of ~(143)Nd/~(144)Nd and a relatively high Pb isotopic composition.
通过对藏北祖尔肯乌拉山地区新生代高钾钙碱岩系火山岩Sr,Nd,Pb同位素成分的系统测试分析表明,火山岩具有相对高的87Sr/86Sr和低的143Nd/144Nd值及高的Pb同位素组成特点,且Sr,Nd,Pb同位素比值变化范围很窄,反映了其具有同源岩浆的特点,并且经历了类似的地球化学动力学过程。
6) high-K calc-alkaline volcanic rocks
高钾钙碱性火山岩
1.
Major and trace elements and Sr-Nd isotope data of adakitic high-K calc-alkaline volcanic rocks in Chibzhang Co area are presented, which yield ages of 35~40 Ma.
常量、微量及Sr、Nd同位素研究表明,藏北赤布张错地区分布的一套始新世(35~4 0Ma)高钾钙碱性火山岩具有C型埃达克岩的地球化学特征。
补充资料:过氧化单硫酸钾与硫酸二钾和硫酸氢钾的化合物
CAS:37222-66-5
中文名称:过氧化单硫酸钾与硫酸二钾和硫酸氢钾的化合物
英文名称:Peroxymonosulfuric acid, monopotassium salt, mixture with dipotassium sulfate and potassium hydrogen sulfate; potassium peroxymonosulfate sulfate,(2khso5.khso4.k2so4); Peroxymonosulfuric acid,monopotassium salt,mixture with dipotassium sulfate and potassium hydrogen sulfate
中文名称:过氧化单硫酸钾与硫酸二钾和硫酸氢钾的化合物
英文名称:Peroxymonosulfuric acid, monopotassium salt, mixture with dipotassium sulfate and potassium hydrogen sulfate; potassium peroxymonosulfate sulfate,(2khso5.khso4.k2so4); Peroxymonosulfuric acid,monopotassium salt,mixture with dipotassium sulfate and potassium hydrogen sulfate
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