1) Guixi rift
桂西裂谷
1.
From the available gravity and magnetic data in combination with other geophysical and geological information,this paper deals with the Guixi rift.
从已有的重力资料出发,结合其他地球物理及地质资料对桂西裂谷进行了探讨。
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) 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。
4) Shanxi rift belt
山西裂谷带
5) 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。
6) West Hill palaeorift
西山古裂谷
补充资料：皖西大裂谷
皖西大裂谷
皖西大裂谷，位于六安市金安区张店镇。地处大别山脉，刘邓大军挺进大别山时，最重要的一次战役—店战役，就发生在此地。现仍保存有许多革命遗迹，可供游客参观凭吊，是大别山红色旅游不可或缺的亮点之一。
皖西大裂谷原名避王岩。源于明末清初农民起义军首领张献忠,在六安地区流动作战的史实和民间传说。相传号称八大王的张献忠，为躲避清军围堵，发现了这一易守难攻的天然屏障，于是率领残部，藏兵于此。现景区内仍遗存有三道关隘闸口、点将台、屯粮洞、避王岩等遗迹。
穿越大裂谷，你会领略到大自然的鬼斧神工。一线天、点将台、石窟王宫（避王岩）、清水潭、蘑菇石、三道闸、回音壁、藏宝阁、窥天崖、云梯、雄起岩等景点，无不让人称奇叫绝，到处可见怪石嶙峋，泉水淙淙，奇花异草，秀竹红枫，飞禽走兽，此乃是集观光、探险、避暑、健身、度假于一体的极佳旅游目的地。
大裂谷外的景区的主要景点有：红色旅游胜地——张家店战役旧址（张家店战斗及革命烈士纪念碑）、江淮第一圩——刘大圩庄园（著名清朝爱国将领、台湾首任巡抚刘铭传旧居）、皖西最大岩洞——敞岩（地处洪山寨风景区），上述景点距大峡谷仅有15分钟以内车程，各处皆令人叹为观止。
青山绿水红土地，美景佳话献给您。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。