1) Amugang accretionary complex
阿木岗增生杂岩
2) accretionary complexes
增生杂岩
1.
Discovery and geologic significance of Late Paleozoic accretionary complexes in central Qiangtang, northern Tibet, China
藏北羌塘中部晚古生代增生杂岩的发现及其地质意义
3) Amugang
阿木岗
1.
Amugang early Yanshan granitoid in Shuanghu area of Tibet Qiangtang basin crop out in the eastern central uplift zone of Qiangtang basin.
西藏羌塘盆地双湖地区阿木岗燕山早期花岗岩体出露于羌塘盆地中央隆起带之东段。
4) Amugang Group
阿木岗群
1.
The age of the Chert Member of the Amugang Group in Qiangtang,Ti bet;
西藏羌塘阿木岗群硅质岩段时代归属
2.
The Amugang Group there is believed to be the Precambrian or pre-Devonian basement of the Qiangtang block, and the Chasang Group, Lugu Formation, etc.
本次工作在阿木岗群和鲁谷组中分别发现中-晚三叠世放射虫化石组合;在查桑群中发现二叠纪中-晚期放射虫化石组合。
6) granitic complex
花岗杂岩
1.
SHRIMP U-Pb dating of zircons from Late Yanshanian granitic complex in Xiaoxinancha gold-rich copper orefield of Yanbian and its geological implications;
延边小西南岔富金铜矿田燕山晚期花岗杂岩的锆石SHRIMP U-Pb年龄及其地质意义
2.
Meanwhile, on the basis of geology and geochemistry characteristics and chronology data, the granitic complex can be divided into three parts: Late Archaean TTG complex, Indosinian adamellitic complex and Yanshanian granitic complex.
通过详细的区域地质研究 ,将阜新地区划分为两个大的构造岩浆带和两个稳定构造区 ,并依据地质、地球化学特征和年代学资料 ,把发育于不同构造单元中的花岗杂岩区分为新太古代TTG杂岩、印支期二长花岗质杂岩和燕山期花岗杂岩 ,同时还讨论了不同时代花岗杂岩的成因。
3.
The Mesozoic intermediate - acidic granitic complexes exposed in eastern Jiaodong area, the eastern part of Shandong Peninsula, contain abundant inclusions of finegrained diorite.
出露在胶东东部地区的中生代中酸性花岗杂岩，普遍含有大量的细粒间长岩类包体。
补充资料：杂阿毗昙心论
【杂阿毗昙心论】
（书名）杂者，杂糅之义，谓于本论杂糅解释也。即法胜阿毗昙心论之释，法救尊者造，十一卷，刘宋僧伽跋摩译。
（书名）杂者，杂糅之义，谓于本论杂糅解释也。即法胜阿毗昙心论之释，法救尊者造，十一卷，刘宋僧伽跋摩译。
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