机译:华北克拉通太行山中生界紫金观基性镁铁质岩浆的成因:岩石学和Os-Nd-Sr同位素约束
Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, PR China;
rnKey Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, PR China;
rnInstitute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 2-15 Natsushima, Yokosuka, 237-0061, Japan;
rnKey Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, PR China;
mafic pluton; petrology; Os-Nd-Sr isotopes; north china craton;
机译:华北克拉通南部太行造山带中生代侵入岩的成岩作用:元素和Sr-Nd-Pb同位素约束
机译:华北克拉通南部太行造山带中生代侵入岩的成岩作用:元素和Sr–Nd–Pb同位素约束
机译:华北克拉通太行-燕山中生代造山带登扎子A型岩浆的成因
机译:硅质熔融橄榄岩的相互作用:对华北克拉通中生代高镁闪长岩的成岩作用和岩石圈演化的制约
机译:华盛顿州北喀斯喀特峰顶岩体的岩石学和岩石成因。
机译:华北太行山中纬度地区冬季土壤CO2通量
机译:五河复合变质基底的锆石U-pb年代学,地球化学和sr-Nd-pb同位素:华北克拉通东南部新太古代活动大陆边缘的影响及中生代花岗岩成因的制约