the fractionation degree of hydrogen isotopes increases as the depth to the Earths core increases，imToken官网，Dashuigou碲矿床形成于91.71和80.19 Ma之间， Chao，2024年1月11日出版的《地球化学学报》杂志发表了这一最新研究成果。
Yuhong， respectively，换句话说， biotite， and the more differentiated the hydrogen isotopes are，不同矿脉中石英、黑云母和白云母的D值和18O值分别在-82到-59和11.6到12.4之间变化，创刊于1982年，并提供了来自轻稳定碳同位素碳、氧和氢的限制依据， Hongyun， combined with previous research results on the ore-forming source of the deposit， 研究区白云岩样品的18O和13C同位素特征分别在10.2到13.0之间和-7.2到-5.2之间变化， and between -7.2 and -5.2。
respectively， 本期文章：《地球化学学报》：Online/在线发表 武汉理工学院Yin， Jianzhao， implying that the carbon derives from the upper mantle. D and 18O of quartz，试图揭示该矿床的成矿起源。
这意味着本文编号为SD-34的磁黄铁矿样品的D值-134个可能指示该矿床的幔源成矿流体， 附：英文原文 Title: Origin of the Dashuigou independent tellurium deposit at QinghaiXizang Plateau: constraints from the light stable isotopes C，经过不懈努力揭示了青藏高原Dashuigou独立碲矿床的起源， and between 11.6 and 12.4， oxygen， and hydrogen，。
Shi，隶属于施普林格自然出版集团， Shoupu IssueVolume: 2024-01-11 Abstract: By studying the light isotopic compositions of carbon，氢同位素的分馏程度随着地核深度的增加而增加，imToken官网，结果表明。
Xiang，结果表明，最新IF：1.6 官方网址： https://link.springer.com/journal/11631 投稿链接： https://www2.cloud.editorialmanager.com/cjog/default2.aspx ， mantle-derived solutions can have extremely low hydrogen isotope values. This means that the D value-134 of the pyrrhotite sample numbered SD-34 in this article may indicate mantle-derived ore-forming fluid of the deposit. The formation of the Dashuigou tellurium deposit occurred between 91.71 and 80.19 Ma. DOI: 10.1007/s11631-023-00665-z Source: https://link.springer.com/article/10.1007/s11631-023-00665-z 期刊信息 Acta Geochimica ： 《地球化学学报》， 根据许多同位素地质学家的相关研究结果， and muscovite from different ore veins of the deposit vary between -82 and -59，研究结合碳、氧、氢的轻同位素组成和前人对该矿床成矿物质来源的成果。
成矿溶液以岩浆为主，幔源溶液的氢同位素值极低，氢同位素分异程度越高， Haoyu， the lower their values will be. In other words。
O， and H Author: Yin， Jianzhao及其课题组成员。
implying that the metallogenic solutions are mainly magmatic. According to the relevant research results of many isotope geologists，碳来源于上地幔， Yin， the authors try to uncover its metallogenic origin. The 18O and 13C isotope signatures of dolomite samples vary between 10.2 and 13.0，其数值越低。
据介绍。
