2) leucogranite
淡色花岗岩
1.
The discovery of Paleozoic leucogranite in eastern segment of Chinese Middle Tianshan and its tectonic implications.;
中天山东段古生代淡色花岗岩的发现及其构造意义
2.
U-Pb zircon age of leucogranite in the central Gangdise, Tibet, and its geological significance;
西藏冈底斯中部淡色花岗岩锆石U-Pb年龄及其地质意义
3.
This pluton exhibits five lithological zones, which, gradational from the lowest level upwards, are leucogranite (zone a), amazonite-bearing granite (zone b), amazonite granite (zone c), topaz-bearing amazonite granite (zone d) and topaz albite granite (zone e).
6Ma,从下至上可分为5个连续过渡的岩相带,即淡色花岗岩(a带),含天河石花岗岩(b带),天河石花岗岩(c带),含黄玉天河石花岗岩(d带)以及黄玉钠长花岗岩(e带)。
3) leucogranites
淡色花岗岩
1.
Leucogranites, distributed in the core or detachment of the MCC, form the famous northern Himalayan leucogranites belt.
藏南拉轨岗日带展布着串珠状变质核杂岩,其内出露的淡色花岗岩体构成北喜马拉雅淡色花岗岩带。
2.
The Higher Himalayan leucogranites in the region of Dinjie, Tibet, are closely near theinner South Tibet Detachments and occur in a series of small stocks.
摘 要西藏定结地区高喜马拉雅淡色花岗岩体紧靠藏南拆离断层内部呈小型岩株产出,多数岩体侵入于基底副变质岩中,大量呈网脉状、似层状及囊状产出的淡色花岗岩脉体亦分布于基底副变质岩中。
4) high Himalaya
高喜马拉雅
5) High Himalayan
高喜马拉雅
1.
The metamorphism and granitic features of the north Himalayas and their comparision with that of the high Himalayan belt REN Liudong;
北喜马拉雅变质作用和花岗岩研究及其与高喜马拉雅结晶岩系的对比
2.
Their veins were widespreadly formed in the basal parametamorphic rocks of the High Himalayan crystallines and the hypersthene granulite restites were found in these veins.
西藏定结地区高喜马拉雅隆起带中淡色花岗岩体紧靠藏南拆离断层内呈等轴状小岩株产出。
6) Higher Himalaya
高喜马拉雅
1.
In the Himalaya orogenic belt,Higher Himalaya crystalline between the north dipping main central thrust fault and the north dipping Rongbushi normal fault (or Southern Tibet detachment system) yields ductile extrusion in wedge shape.
在喜马拉雅造山带 ,高喜马拉雅结晶地体沿北倾的主中央逆冲断层和北倾的绒布寺正断层 ,表现为相对刚性体之间的韧性体的楔状挤出。
2.
The major constraints of the processes of muscovite granite for-mation, taking the Higher Himalaya for an example, are demostrated from multiple-aspect of geology, petrology, geochemistry, experimental petrology and geophysics.
以高喜马拉雅地区为例,从地质学、岩石学、地球化学、实验岩石学和地球物理学等多方位论述了白云母花岗岩形成过程的主要约束,提出并论证一个比较合理的陆内俯冲带热结构与白云母/二云母花岗岩形成的成因模型。
补充资料：色喜
1.喜悦流露在脸上。
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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