2) Wuchuan-Sihui fault zone
吴川-四会断裂带
1.
During the Caledonian period,the embryonic form of the Wuchuan-Sihui fault zone began to form, which was companied by the planar greenschist facies metamorphism,but without the primary gold enrichment.
加里东期，吴川─四会断裂带雏形开始形成，但金并未得到初步富集。
3) Wuchuan-Sihui Fault
吴川-四会断裂
1.
The Wuchuan-Sihui fault is an important deep-seated fault and ore-controlling structurein South China.
吴川－四会断裂是我国华南一条重要的深大断裂兼控矿构造，沿带分布了一系列大型、超大型金属矿床，同时与粤北铀矿成矿有着十分密切的关系。
4) Wuchuan-sihui tectonic belt
吴川-四会构造带
5) The Sihui-Wuchuan fracture
四会-吴川断裂
6) The learned society of Wuyue history and geography
吴越史地研究会
1.
The learned society of Wuyue history and geography , which studied area culture, is the first civil academic institution in China\'s modern history.
吴越史地研究会是中国近代史上较早的研究区域文化的民间学术机构。
补充资料：吴会
1.秦汉会稽郡治在吴县，郡县连称为吴会。 2.东汉分会稽郡为吴会稽二郡，并称吴会。后亦泛称此两郡故地为吴会。
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