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1)  EMⅡ mantle source
EMⅡ型地幔源区
2)  Mantle source region
地幔源区
3)  Mantle source
地幔源区
1.
Characteristics of mantle source for Jining Cenozoic basalts from southern Inner Mongolia:evidence from element and Sr-Nd-Pb isotopic geochemistry.Acta Petrologica;
内蒙古集宁新生代玄武岩的地幔源区特征:元素及Sr-Nd-Pb同位素地球化学证据
2.
All these features indicate consistently that the ore-bearing magma was derived from an enriched lithospheric mantle source which had been metasomatized by the subducted sedimentary melt,and that the magma originated from a source with low extent of partial melting (about 10%) at a shallow depth of the spinel lherzolite facies.
这些特点一致反映出含矿岩浆产生于受俯冲沉积物熔体交代的富集型岩石圈地幔源区。
4)  Mantle source characteristics
地幔源区特征
1.
Mantle source characteristics of magmatic carbonatites from the Himalayan Collision Zone in western Sichuan,SW China:Evidence of Pb-Sr-Nd isotopes.;
川西喜马拉雅期碰撞造山带岩浆碳酸岩的地幔源区特征——Pb-Sr-Nd同位素证据
5)  mantle source rock
地幔源岩
6)  inhomogeneity of the mantle source
地幔源区不均一性
补充资料:[3-(aminosulfonyl)-4-chloro-N-(2.3-dihydro-2-methyl-1H-indol-1-yl)benzamide]
分子式:C16H16ClN3O3S
分子量:365.5
CAS号:26807-65-8

性质:暂无

制备方法:暂无

用途:用于轻、中度原发性高血压。

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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