1) U-Pb zircon dating
锆石U-Pb法定年
2) zircon
锆石
1.
Collation of age of ore-hosting volcanics in Xiongcun superlarge Cu-Au deposit on basis of three zircon U-Pb SHRIMP ages;
三个锆石U-Pb SHRIMP年龄对雄村特大型铜金矿床容矿火成岩时代的重新厘定
2.
Relationship between Gangdese porphyry copper deposits and uplifting of southern Tibet plateau: Evidence from multistage zircon of ore-bearing porphyries;
冈底斯斑岩铜矿与南部青藏高原隆升之关系——来自含矿斑岩中多阶段锆石的证据
3.
A SHRIMP U-Pb chronological study of zircons from quartz veins of Yangshan gold deposit, Gansu Province;
甘肃省阳山金矿床石英脉中锆石SHRIMP U-Pb年代学研究
3) baddeleyite and zircon
斜锆石与锆石
1.
Difference in U-Pb isotope ages between baddeleyite and zircon in metagabbro from the Fushui complex in the Shangnan-Xixia area,Qinling orogen;
秦岭造山带商南—西峡地区富水杂岩的变辉长岩中斜锆石与锆石U-Pb同位素年龄的差异
4) hydrothermal zircon
热液锆石
1.
Unfortunately, hydrothermal zircons that grow directly from mineralizing fluids and inherited magmatic or metamorphic zircons from wall rocks may .
近年来同位素质谱技术的发展使得通过含金石英脉中热液锆石的U-Pb定年来精确限定石英脉型金矿床成矿时代成为可能。
5) zircon SHRIMP
锆石SHRIMP
1.
Based on previous research and zircon SHRIMP data,the authors suggest that the "Dahalajunshan Formation" should be disintegrated into several different formations.
基于前人的资料和本文获得的锆石SHRIMP数据,故建议解体“大哈拉军山组”。
6) zircon corundum
锆石刚玉
参考词条
补充资料：钙钠锆石
分子式： (Na, Ca)3Zr[Si2O7](O,F)2
CAS号：
性质：常含锰、铌、钛等。晶体呈柱状或板状；也成不规则粒状。莫氏硬度6。相对密度3.5～3.6。玻璃光泽。黄色或红褐色。条痕黄色。微透明。性脆。解理平行，轴面中等。断口参差状。见于碱性岩中。是提炼锆的矿物原料。
CAS号：
性质：常含锰、铌、钛等。晶体呈柱状或板状；也成不规则粒状。莫氏硬度6。相对密度3.5～3.6。玻璃光泽。黄色或红褐色。条痕黄色。微透明。性脆。解理平行，轴面中等。断口参差状。见于碱性岩中。是提炼锆的矿物原料。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。