1)  U-Pb
U-Pb
1.
Through highly precise dating of the ages of petrogenesis and mineralization of the tungsten deposit,the authors obtained a SHRIMP U-Pb zircon age of 156.
笔者对其含矿岩体和矿石进行了成岩成矿年龄精测,分别获得细粒似斑状白云母花岗岩锆石SHRIMP U-Pb年龄为(156。
2.
The authors have conducted geochronological study on the samples from the ore-bearing porphyry and orebodies by SHRIMP zircon U-Pb and molybdenite Re-Os dating,respectively.
本文利用SHRIMP锆石U-Pb和辉钼矿Re-Os同位素对含矿斑岩体和矿石进行了精细成岩成矿时代测定,获得钾长花岗斑岩的SHRIMP锆石U-Pb年龄为224。
3.
Based on the geological,petrological and geochemical characteristics,the SHRIMP zircon U-Pb ages, of the Mashan and Xueshan granitoids,two main geological units of the Yishui Magmatic Complex,are reported.
本文在简要介绍这两个岩体的基本地质、岩石化学和地球化学特征的基础上,首次报道了这两个岩体的SHRIMP锆石U-Pb定年结果。
2)  U-Pb
铀-铅
3)  U-Pb SHRIMP dating
U-Pb SHRIMP定年
4)  U-Pb dating
U-Pb定年
1.
Formation time and magma source of granites in Bengbu uplift: Evidence from LA-ICPMS zircon U-Pb dating and tracing;
蚌埠隆起区花岗岩形成时代及岩浆源区性质:锆石LA-ICPMS U-Pb定年与示踪
2.
Timing of the Hong′an Group in Hubei:Constraints from U-Pb dating of metagranitic intrusions;
湖北红安群的时代:变质花岗质侵入体U-Pb定年提供的制约
3.
Recent development in mass spectrometry makes it possible to determine the age of auriferous quartz veins by U-Pb dating of zircons from quartz veins.
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 U-Pb age
锆石U-Pb年龄
1.
Zircon U-Pb age and Hf isotopic composition of the Xiaozhangjiakou ultramafic pluton in northern Hebei;
冀北小张家口超基性岩体的锆石U-Pb年龄和Hf同位素组成
2.
Zircon U-Pb ages,Hf isotopic characteristics and their implications of the Early Paleozoic granites in the northeastern Da Hinggan Mts.,northeastern China;
大兴安岭东北部早古生代花岗岩锆石U-Pb年龄、Hf同位素特征及地质意义
3.
Zircon U-Pb age, Sr-Nd-Pb isotopic compositions and trace element of Fangshan complex in Beijing and their petrogenesis significance.;
北京房山岩体锆石U-Pb年龄和Sr、Nd、Pb同位素与微量元素特征及成因探讨
6)  zircon U-Pb dating
锆石U-Pb定年
1.
In order to determine the formation age of the Hongshan topaz-bearing granite and make metallogenic potential prognosis, the authors carried out LAM-ICPMS zircon U-Pb dating and detailed geochemical comparison.
对闽西南红山含黄玉花岗岩进行了LAM-ICPMS锆石U-Pb定年以及地球化学对比研究。
2.
Zircon U-Pb dating yields 219.
单颗粒锆石U-Pb定年结果为219。
3.
Using TIMS zircon U-Pb dating method,the author measured the isotope age of quartz-biotite-diorite from the Jiuxiantang intrusion during the regional geological investigation of 1∶250000 scale Shanggao county sheet.
笔者在该区进行1∶25万上高县幅区域地质调查时,利用TIMS锆石U-Pb定年方法对九仙汤英云闪长岩进行了同位素年龄测定,结果表明九仙汤侵入体形成时代为(763±1)Ma,属新元古代花岗岩。
参考词条
补充资料:[N,N-bis[2-[bis(carboxymethyl)amino]ethyl]glycinato(5-)]-, diammonium, (PB-7-13-12564)-Ferrate(2-)
CAS: 85959-68-8
分子式: C14H18FeN3O10·2H4N

中文名称: N,N-二[2-[二(羧甲基)氨基]乙基]甘氨酸基合铁(2-)二胺盐

英文名称: [N,N-bis[2-[bis(carboxymethyl)amino]ethyl]glycinato(5-)]-, diammonium, (PB-7-13-12564)-Ferrate(2-)
ferrate(2-), [rel-[n(r)]-n-[2-[bis[(carboxy-.kappa.o)methyl]amino-.kappa.n]ethy
l]-n-[2-[(s)-[(carboxy-.kappa.o)methyl](carboxymethyl)amino-.kappa.n]ethyl]glyc
.kappa.o]-, diammonium, (pb-7-13-12564)-inato(5-)-.kappa.
Ferrate(2-),[N,N-bis[2-[bis(carboxymethyl)amino]ethyl]glycinato(5-)]-,diammonium,(PB-7-13-12564)-



说明:补充资料仅用于学习参考,请勿用于其它任何用途。