1) Gangdise island arc belt
冈底斯南缘火山-岩浆弧带
1.
Discovery and geological significance of the adakite in Gangdise island arc belt,Xizang(Tibet).;
西藏冈底斯南缘火山-岩浆弧带中桑日群adakite的发现及其意义
2) Gangdise volcanic-magma arc
冈底斯火山-岩浆弧
3) Gangdise magmatic arc
冈底斯岩浆弧
1.
The geology and tectonic implications for the Paleogene bimodal volcanic rocks in the middle part of the Gangdise magmatic arc, southern Xizang;
冈底斯岩浆弧中段古近纪“双峰式”火山岩的地质特征及其构造意义
4) Gangdise magma arc
冈底斯岩浆弧
1.
Holocene volcanic rocks are found in the Gangdise magma arc and a group of isotopic dating data are obtained, which further enriches the temporal-spatial framework of the magmatic evolution in Gangdise.
在冈底斯岩浆弧中新发现第四纪全新世火山岩,获取一批同位素定年资料,进一步丰富了冈底斯岩浆演化的时空格架。
2.
Relics of the Late Triassic Parlung Zangbo ophiolitic mélange belt are found in the traditional Gangdise magma arc and it has been demonstrated that the Middle Jurassic mottled conglomerate unconformably overlies the strata on both sides of this ophiolitic mélange belt.
在传统的冈底斯岩浆弧中新发现一条时代为晚三叠世的迫龙藏布蛇绿混杂岩带,并查明中侏罗世杂色砾岩角度不整合覆盖在该蛇绿混杂岩带两侧的地层之上,表明冈底斯岩浆弧中有一条印支晚期叠合的缝合带。
3.
Recent study has confirmed that there exists a porphyry-type Cu (Mo ,Au )polymetallic met-allogenic belt along the Gangdise magma arc in the southern Qinghai-Tibet Plateau.
近年来发现青藏高原南部冈底斯岩浆弧中发育了一条潜力很大的斑岩型铜(钼、金)多金属成矿带。
5) continental-margin volcanic-magmatic arc zone
陆缘火山-岩浆弧带
1.
The delineation and significance of the continental-margin volcanic-magmatic arc zone in the northern part of the Bangong-Nujiang suture zone;
班公湖-怒江结合带北侧陆缘火山-岩浆弧带的厘定及其意义
6) Gangdese island-arc magma
冈底斯岛弧岩浆岩
补充资料：上南冈
【诗文】：
暮坞屋荒凉，寒陂水清浅。
捐书息微倦，委辔随小蹇。
偶攀黄黄柳，却望青青巘。
幽寻复有兴，未觉西林晚。
【注释】：
【出处】：
暮坞屋荒凉，寒陂水清浅。
捐书息微倦，委辔随小蹇。
偶攀黄黄柳，却望青青巘。
幽寻复有兴，未觉西林晚。
【注释】：
【出处】：
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