1) Chencai Group in west Zhejiang
浙西陈蔡群
2) chencai group
陈蔡群
1.
Structural analysis lndicates that Chencai group in the southwestern Zhejiang province was experienced five eplsodes of structural deformations.
构造解析表明浙西南陈蔡群曾遭受5期构造变形叠加改造。
2.
In this paper,the amphibolites in Chencai group metamorphic rocks have been studied by means of geochemistry.
本文对陈蔡群变质岩中的斜长用闪岩进行了地球化学研究。
3.
The main body of the origional rocks of Chencai group was formed in ocean island,compsed of tholeiite and cognate gabbro, Carbonatite and argillo-arenaceous clastic rocks of turbidity current deposition.
陈蔡群原岩的主体形成于大洋岛弧环境，由拉斑玄武岩和同源辉长岩，碳酸盐岩和浊流沉积的泥砂质碎屑岩组成；经受了中压角闪岩相区域动力—热流变质作用和多期褶皱变形；岩石地球化学和同位素年代资料表明，中国东南的威尔逊旋回在中元古晚期便已开始，即那时于扬子古陆与华夏地块之间存在一大洋盆地，洋壳上可能存在拉张期残留的花岗质陆壳碎块。
3) Chencai Khondalite series
陈蔡群孔兹岩
1.
The metamorphic formation of Chencai Khondalite series is predominant of gneisses、with some amphibolites、leplites、quartz schists and marbles.
本文对浙江陈蔡群孔兹岩系的变质岩石组合、原岩建造、变质作用、成矿作用以及地壳早期历史的演化进行了研究。
4) Chencai Reservoir
陈蔡水库
1.
Water Source Protection and Countermeasures of Chencai Reservoir
陈蔡水库水源保护与防治对策研究
5) western Zhejiang
浙西
1.
This paper introduced the achievements of the 1: 50, 000 regional geological surveying in shiershan granite areas of Western Zhejiang, which was conducted with the theory of "granite superunit - unit" recently.
本文介绍近年来在浙西石耳山花岗岩区引进“花岗岩超单元─单元”理论进行的1：5万区域地质调查工作取得的成果。
2.
Because of facies difference,black carbonaceous shale and fine-grained siliciclastic sequences at the lower part of the Cambrian exhibit various changes in southern Anhui and western Zhejiang areas.
皖南和浙西地区寒武系下部黑色岩系地层发育差异明显,常见的岩石地层单位为黄柏岭组和荷塘组。
6) Cai Xishan's Mai jing (Pulse Classic)
蔡西山《脉经》
补充资料：晚春宴无锡蔡明府西亭
【诗文】：
茅檐闲寂寂，无事觉人和。井近时浇圃，城低下见河。
兴缘芳草积，情向远峰多。别日归吴地，停桡更一过。
【注释】：
【出处】：
全唐诗：卷206_23
茅檐闲寂寂，无事觉人和。井近时浇圃，城低下见河。
兴缘芳草积，情向远峰多。别日归吴地，停桡更一过。
【注释】：
【出处】：
全唐诗：卷206_23
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