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1)  hyperbasite complex
超基性杂岩
1.
These processes resulted in the formation of peculiar dunites in the hyperbasite complexes (chromite ores),development of low sulfide horizons and hortonolite dunites .
这些作用导致产在超基性杂岩中的特殊纯橄榄岩(铬矿石)、基性超基性层状侵入体中的低硫层和铁镁橄榄石纯橄榄岩(铂族金属矿床)的形成,以及富铁火成分异岩的透岩浆硫化作用(CuNi硫化物和CuZnPb硫化物矿石)。
2)  ultramafic alkaline complexes
超基性碱性杂岩
3)  ultrabasic complex
超基性岩-碳酸岩杂岩体
1.
A super-large vermiculite-apatite deposit originated from the Qieganbulak ultrabasic complex and located at Southern Kuluketage fault block,northeastern margin of Tarim.
产有超大型蛭石-磷灰石矿床的且干布拉克超基性岩-碳酸岩杂岩体位于塔里木板块东北缘库鲁克塔格断隆南侧。
4)  Alkaline-ultrabaio rock complex body
碱性超基性岩杂岩体
5)  basicultrabasic complex belt
基性-超基性杂岩带
6)  alkali-ultrabasic complex
碱性超基性杂岩体
1.
Writers are taken that the vermiculite ore deposit exists in the alkali-ultrabasic complex in Yuli Xinjiang as the example, contrast it with same deposits at home and abroad, and find its inhere law and establish the metallogenic model.
以新疆尉犁碱性超基性杂岩体中超大型蛭石矿床为例,通过与国内外同类型矿床对比,建立了矿床成因模式,揭示出其内在的规律,为寻找与深入研究同类矿床提供了依据。
补充资料:5,5-二丁基-12-乙基-9-氧代-10-氧杂-4,6-二硫杂-5-锡杂十六烷酸-2-乙基己基酯
CAS:53202-61-2
分子式:C30H60O4S2Sn

中文名称:5,5-二丁基-12-乙基-9-氧代-10-氧杂-4,6-二硫杂-5-锡杂十六烷酸-2-乙基己基酯

英文名称:10-Oxa-4,6-dithia-5-stannahexadecanoic acid, 5,5-dibutyl-12-ethyl-9-oxo-, 2-ethyl-hexyl ester
6-dithia-5-stannahexadecanoic acid, 5,5-dibutyl-12-ethyl-9-oxo-10-oxa- 2-eth
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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