1) U-Th-Pb bearing accesory mineral
U-Th-Pb副矿物
2) Mineral U-Th isochron
U-Th矿物等时线
1.
Mineral U-Th isochron systematic is a popular method in young volcanism (＜350ka) dating,based on U-series disequilibrium.
U-Th矿物等时线法定年适用于小于350ka范围的年轻火山岩。
3) Combined U-Th-Pb-Sm-Nd dating technique
U-Th-Pb-Sm-Nd联合定年
4) Th-U-total Pb dating
Th-U-Pb化学法定年
5) EMPA monazite Th-U-Pb chemical dating
独居石电子探针Th-U-Pb化学法定年
1.
Detailed SHRIMP and LA-ICPMS zircon U-Pb isotopic dating and EMPA monazite Th-U-Pb chemical dating revealed the zircon and monazite geochronology of three blocks.
较为详细的SHRIMP、LA-ICPMS锆石U-Pb年代学和独居石电子探针Th-U-Pb化学法定年揭示,隆化-凤山地块的石英闪长质片麻岩和石榴黑云二长花岗质片麻岩分别形成于2484Ma和2180Ma,同时存在3164～2553Ma的锆石记录和约1854Ma的变质改造事件;细粒二长花岗岩形成于413Ma,独居石内核记录了约628Ma的继承年龄。
6) geochemistry of U and Th
U、Th迁移
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
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。
参考词条