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1)  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。
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 Group in west Zhejiang
浙西陈蔡群
4)  khondalite
孔兹岩系
1.
Studies on mineralogy and petrology of khondalite in Helan Mountain indicate that the typical metamorphic minerals such as garnet biotite and cordierite have good correlations with the adjacent equivalents, but the correlation between the typical minerals and the host rocks is not apparent.
贺兰山北段孔兹岩系详细的岩石学和矿物学的研究表明 ,岩石中的特征变质矿物如石榴子石、堇青石等的成分与其周围相邻的同世代变质矿物具有很好的相关性 ,而与其寄生主岩成分的相关性较小 ,而贯通矿物如斜长石却与其寄生主岩成分的相关性较为密切 ,同时天然块状样品的脱水熔融实验的结果也显示 ,变质反应是在一个局部平衡体系中进行的。
2.
The garnet migmatitic granite (GMG) was formed by partial melting of Ga-Bi gneiss within Ga-Bi gneiss complex of Archaean khondalites in Daqingshan area, Inner Mongolia, in the process of subhorizontal shearing and granulite facies metamorphism.
内蒙古大青山地区太古宙孔兹岩系在发生麻粒岩相变质作用的同时,榴云片麻岩岩组中的石榴黑云片麻岩在近水平剪切构造变形过程中发生部分熔融,形成了石榴混合花岗质岩石。
3.
Early Precambrian metamorphic complex, composed of khondalite series, BiHb gneiss series, granulite series and metamorphosed plutonic intrusions inside the supracrustal rocks, are well developed in Daqingshan area.
内蒙古大青山地区普遍发育由孔兹岩系、黑云角闪片麻岩系、麻粒岩系和侵位其中的变质深成岩构成的高级变质杂岩。
5)  khondalite series
孔兹岩系
1.
Geochemical characteristics and protoliths of the marble rock group of the khondalite series in the Daqing Mountains, Inner Mongolia;
内蒙古大青山地区孔兹岩系中大理岩岩组的地球化学特征及原岩建造
2.
Structure of metamorphic strata of the khondalite series in the Daqingshan-Wulashan area,central Inner Mongolia,China,and their geodynamic implications.;
内蒙古中部大青山—乌拉山地区孔兹岩系的变质地层结构及动力学意义
3.
Khondalite series — geochronology and geochemistry of the Jiehekou Group in Luliang area, Shanxi province.;
孔兹岩系——山西吕梁地区界河口群的年代学和地球化学
6)  khondalite
孔兹岩
1.
Discussion on the Age of Khondalite in Jin Meng (Shanxi Nei Mongol) High Grade Terrain;
晋蒙高级地体孔兹岩系的时代
2.
Discussion on the Early Precambrian Grey Gneiss and Khondalite in Nei Mongol Shanxi Hebei Junction Region, North China;
关于内蒙与晋冀交界地区早前寒武纪灰片麻岩和孔兹岩的讨论
3.
This ductile shear zone is composed of 7 km-wide mylonitized khondalites.
在青藏高原西昆仑地体南部的元古宙片麻岩穹窿南侧 ,发育一条近 EW向规模巨大的康西瓦韧性走滑剪切带 ,韧性剪切带岩石由 7km宽的糜棱岩化的孔兹岩系组成 ,孔兹岩原岩为富铝质泥质沉积岩夹火山岩及大理岩。
补充资料:送陈校书赴蔡州幕
【诗文】:
天假纵横入幕筹,东南顿减一方忧。行赍健笔辞天阁,
坐见妖星落蔡州。青草袍襟翻日脚,黄金马镫照旄头。
此行领取从军乐,莫虑功名不拜侯。



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【出处】:
全唐诗:卷506-43
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