1) Nielamu Group
聂拉木群
1.
Because these values match the isotropic composition of the paragneisses in Nielamu Group distributed along High Himalayas, they are regarded as the most probable parental rocks of Yadong leucogranite.
Rb-Sr和Sm-Nd同位素组成显示亚东淡色花岗岩的源岩很可能是聂拉木群副变质岩。
2) Nyalam Group-complex
聂拉木岩群
1.
The in tegrated meta morphic plu tonic rocks are called the Sima gneiss,which was emplaced in the Jin ningian Stage;whereas the metamorphic strata are called the Nyalam Group-complex,in cluding the Quxam and Jiangdong Formation-com plexes.
变质地层称聂拉木岩群,包括曲乡岩组和江东岩组,两者以韧性断层接触,沉积时代为古元古代,经历了吕梁末期的中压型蓝晶石—十字石亚相区域动力热流变质作用,并与思马片麻岩一同于晋宁末期接受角闪岩相变质、喜马拉雅期绿片岩相退变质。
3) Nyalam
聂拉木
1.
Magnetic fabrics and tectonic implications of the Higher Himalayan rocks in Nyalam, southern Tibet;
聂拉木地区高喜马拉雅岩石磁组构及其构造含义
2.
Precambrian crystalline basement in the Nyalam region,southern Xizang;
西藏南部聂拉木地区前寒武纪结晶基底的组成及其特征
3.
The Charceteristics and Significances of the Fills in the Incised Valleies of Naxing Formation Near North Nyalam,Tibet;
西藏聂拉木地区纳兴组深切谷充填序列特征及意义
4) Nieniexiongla
聂聂雄拉
1.
The strata of early and middle Jurassic epoches are relatively developed in Nieniexiongla region, Nyalam County, Tibet, with various genera and species of fossils.
西藏聂拉木县聂聂雄拉地区 ,早、中侏罗世地层较发育 ,地层中化石属种繁多。
5) the Nyalam area of southern Tibet
西藏南部聂拉木地区
6) Zhamunie
扎木聂
1.
The article gives a brief account of the historical background of its birth from Sajia Dynasty in the 13th century throuh mdti-17th century,its chief accompanying music instrument of Zhamunie,its bright and elegant characteristics and its rich varity etc.
堆谐起源于13世纪萨迦王朝时期,流行于17世纪中叶五世达赖时期,以扎木聂为主要伴奏乐器。
补充资料：多木拉克脱拜古墓群
古墓群位于贝母房子村西，清水沟北岸的农田中，东为一南北向小干沟，南临河谷，北接齐阿思山丘，据推测为唐以前地方民族的墓葬。葬区面积18万平方米，以多木拉克脱拜大墓为主。分布有大小三十余座石堆，石围墓。其中一号大墓—多木拉克脱拜墓底直径46米，残高约8米，顶部偏东北塌陷，墓葬之石块堆积较规则，由底部分层盘旋至顶。底部石块大而多。大墓之东南墓葬分布稀疏，西南则分布稠密，墓与墓之间距离较短。墓群规模均小于大墓，直径约9-18米，残高10-110厘米之间不等，且均有塌陷。
墓群定为昌吉自治州级重点文物保护单位，得到妥善保存。
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