1) basicultrabasic complex belt
基性-超基性杂岩带
2) 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（ＣｕＮｉ硫化物和ＣｕＺｎＰｂ硫化物矿石）。
3) ultrabasic rock belt
超基性岩带
1.
This paper started from olivine and pyroxene,the main rock-forming minerals of mineralized rock bodies in the Longshoushan ultrabasic rock belt, to their mineral-chemistry features and emphasized on the difference and similarity between the Jingchuang rock body and the surrounding rock bodies.
对甘肃龙首山超基性岩带含矿岩体的主造岩矿物———橄榄石、辉石,进行了矿物化学特征分析 ;比较了金川岩体与外围岩体在矿物化学特征方面的异同。
4) Jingbulake
基性-超基性岩带
1.
The basic-ultrabasic rocks of Jingbulake belt are situated within the Nalati fault in southwestern Tianshan,where more than ten intrusions:Jingbulake,Kaladala,Qiagansayi,Qiaoletiekexi,Qiulaketeleke,Sulu,Qiongawuzi,etc.
菁布拉克基性-超基性岩带位于西南天山那拉提深大断裂附近,出露有菁布拉克、喀拉达拉、恰干萨依、乔勒铁克西、丘拉克特勒克、苏鲁、琼阿乌孜等基性超基性岩体。
5) ultrabasic and basic rocks
基性超基性岩带
6) ultramafic alkaline complexes
超基性碱性杂岩
补充资料：连续性与非连续性(见间断性与不间断性)
连续性与非连续性(见间断性与不间断性)
continuity and discontinuity
11an父ux泊g四f“山。麻以角g、.连续性与非连续性(c。nt，n琳t:nuity一)_见间断性与不间断性。and diseo红ti-
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