1) Kangding complex
康定杂岩
1.
The Panxi granulite is the most important part of Kangding complex.
攀西麻粒岩是扬子陆块西缘康定杂岩的重要代表。
2.
The Kangding complex is a S-N trending zone in the western margin of the Yangtze Block.
康定杂岩在扬子地块西缘呈南北向带状分布,这套岩石岩性变化很大(从基性到中性、酸性),中性、酸性岩是组成该杂岩的主体。
3.
Geochemical data indicate that Yajiangqiao trondhjemite, Huatan trondhjemite and Mopanshan granite, considered as component parts of Kangding complex formed in Late Archean or Palaeoproterozoic, are similar to TTG in such aspects as low Mg~#, Na-2O>K-2O, strong fractionationed REE, no or slightly negative Eu anomaly, low Yb-N, Cr, Ni, V, Nb, Ta, Ti, high Ba, and changeable Sr.
对原划为新太古代古元古代康定杂岩的雅江桥片麻状奥长花岗岩、花滩奥长花岗岩和磨盘山花岗岩的地球化学分析表明,其具有低Mg#、Na2O>K2O,轻重稀土元素强烈分异,无或略具微弱的负Eu异常,低YbN、Cr、Ni、V、Nb、Ta、Ti,高Ba,Sr变化较大,与TTG类似。
2) Kangding Group Complex
康定岩群
3) complex
[英]['kɔmpleks] [美][kəm'plɛks, 'kɑm,plɛks]
杂岩
1.
The first disintegration of Altgn Tagh rock group and the characteristics of Altgn Tagh complexes;
“阿尔金群”的解体与阿尔金杂岩特征
2.
This paper mainly discusses the features of the ferroginous ultrabasic basic complex in the deep seated fracture zone between the Penglu terrain and the Zhenggongshan terrain.
本文着重论述了彭庐地体与障公山地体间深断裂带内的铁质超基性－基性杂岩特征。
4) magmatic complex
岩浆杂岩
1.
It is substaintiated that the beding glide fold are dominance in the superficial and the magmatic complex are .
对岩浆杂岩成功地进行了解体，认为侵入岩具多种成因类型并具多旋回演化特点，指出地台边缘的层序地层有别于陆棚边缘经典模式。
5) Graywacke
[英]['greiwæk] [美]['gre,wæk]
杂岩，硬岩
6) Kangding
康定
1.
Assessment of the susceptibility of geological hazards in Kangding county town,western Sichuan;
四川康定城地质灾害易发分区评价
2.
Assessment of the vulnerability of social economy by geological hazards in Kangding county town,western Sichuan;
四川康定城地质灾害社会经济易损性分区评价
3.
Risk assessment of geological hazards in Kangding county town,western Sichuan;
四川康定城地质灾害危险性分区评价
补充资料：杂定
1.共同审定。
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