1) Panzhihua-Xichang rift zone
攀西裂谷带
1.
This paper describes geological features and criteria for ore prospecting of Pt-Pd ore deposits in the Panzhihua-Xichang rift zone by the example of the Nantianwan Pt-Pd deposit,and divides prospective ore-forming areas,pointing out prospecting potential in the Panzhihua-Xichang rift zone.
以南天湾铂钯矿床为例,简述了其地质特征,建立了找矿标志,划分了成矿远景区,并论述了攀西裂谷带铂钯矿的找矿前景。
2) Panxi rift
攀西裂谷
1.
PGE mineralization of layered intrusions in Panxi rift region,China;
攀西裂谷地区层状镁铁岩的PGE矿化作用
2.
It is located in north part and west flank of the Panxi rift and belongs to the western sub-belt of REE mineralization in the west of Mianning region.
木洛稀土矿床是攀西地区新发现的中型稀土矿床,位于攀西裂谷带北段西界,冕西稀土成矿带西部亚带。
3.
It is located in the west fl ank of the Panxi rift, but the REE mineralization was developed in the postrift stage based on the isotopic ages and the geological environment.
四川牦牛坪矿床是世界上最大的稀土矿床之一 ,该矿床位于攀西裂谷西缘 ,同位素年龄表明稀土矿化发育于裂谷期后阶段。
3) Panxi paleorift
攀西古裂谷
1.
Zircon SHRIMP U-Pb dating was performed on alkali feldspar-quartz syenite and arfvedsonite alkali granite in the Cida alkali complex in the Dechang area, in the Panxi paleorift.
对产于攀西古裂谷带内的德昌地区茨达碱性杂岩体中的碱长石英正长岩和钠铁闪石碱性花岗岩进行了锆石SHRIMP U-Pb年龄测定,年龄结果分别为221Ma±6Ma和225Ma±2Ma,表明该碱性岩的结晶年龄或成岩年龄相当于晚三叠世,同时暗示攀西古裂谷的张裂时间为三叠纪。
2.
Yele granite exposed in Yele,Mianning,middle sector of west margin of the Yangtze landmass, is a S type granite It gives an isopotic age value of 350±19Ma,so that it was emplaced in the Early Carboniferous and was a product in prerifting anticline uplift stage of the Panxi paleorift This result fills in the gaps in the Early Carboniferous magmatism in this regio
在岩体中获 350± 19Ma的年龄值 ,表明其侵位时代为早石炭世 ,为攀西古裂谷孕育时期的裂前台背斜隆起阶段的产物。
4) Panxi valley
攀西河谷
1.
It and Italian are suitable to grow at 1 600-2 300m elevation in Panxi valley.
攀西地区气候类型多样,光热充足,适合多种优质牧草生长,对四种牧草营养成分的测定表明,在盛花期紫花苜蓿粗蛋白含量高,占干物质的22 1%以上,是攀西河谷山地主要优质青饲料,它与多花黑麦草适合在攀西河谷海拔1600—2300m地带生长。
5) Shanxi rift belt
山西裂谷带
6) Western margin fault of Gulu Basin
谷露盆地西缘断裂带
补充资料：攀移
攀移
disloeation elimb
、叮刀月火一甲~/攀移disloeation elimb位错离开其滑移面的运动，是位错运动的一种基本形式(见滑移)。它是需要涉及点缺陷(空位或自填隙原子)的远程运动(扩散、聚集或逸去)。所以攀移又称为非保守性运动。例如由一个正刃型位错的附加半原子面的“刃边”移去一行原子(或聚集一行空位)，则此刃型位错离开其滑移而向上攀移一个单元距离，反之则向下攀移一个单元距离。位错攀移常由位错线上割阶或双割阶之形成及沿位错线的横向运动而实现。位错攀移需要点缺陷的长程扩散运动，所以受温度的影响较显著。纯螺型位错由于其伯格斯矢量与位错线平行，所以所有含该位错的平面都是它的滑移面，它也就没有攀移运动。(杨顺华)
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