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Mineralogical and chemical transformations of volcanic ash and rocks through interaction with water: insights into the genesis of lithium deposits in Puna Brines 通过与水的相互作用,火山灰和岩石的矿物学和化学转化:对普纳盐沼锂矿床成因的见解
IF 4.8 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-15 DOI: 10.1007/s00126-026-01428-5
D. A. Del Bono, L. G. Borda, L. V. Godfrey, N. L. Chiaramonte, C. Balbis, A. I. Pasquini, M. G. García
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引用次数: 0
Magmatic evolution and mush processes of the Xiarihamu Ni-Cu deposit: insights from olivine-orthopyroxene-clinopyroxene chemistry 下日哈木镍铜矿床岩浆演化与泥化过程:来自橄榄石-正辉石-斜辉石化学的启示
IF 4.8 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-11 DOI: 10.1007/s00126-025-01421-4
Xu-Yang Zheng, Ya-Jing Mao, Fang-Lin Yuan, Yi Li, Wen-Jun Li, Ke-Zhang Qin
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引用次数: 0
Assessing the geochemical anomalies of bismuth, gallium, indium, and tellurium in the Río Blanco porphyry Cu-Mo deposit, central Chile; implications for the critical mineral and metal potential of porphyry copper systems 智利中部Río Blanco斑岩型铜钼矿床中铋、镓、铟、碲地球化学异常评价对斑岩型铜系统的关键矿物和金属潜力的启示
IF 4.8 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-09 DOI: 10.1007/s00126-025-01422-3
Homayoun Fathollahzadeh, Jorge Crespo Mena, Simon M. Jowitt
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引用次数: 0
Quartz compositions decipher the source and magmatic-hydrothermal evolution of Himalayan LCT-type pegmatites 石英组成揭示了喜马拉雅lct型伟晶岩的来源和岩浆-热液演化
IF 4.8 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-07 DOI: 10.1007/s00126-025-01424-1
Yong-Neng Zhao, Jun-Xing Zhao, Noreen J. Evans, Chang-Tong He, Rui-Zhe Shi, Shen Gao, Li-Qun Zhu, Ke-Zhang Qin, Ming-Jian Cao
{"title":"Quartz compositions decipher the source and magmatic-hydrothermal evolution of Himalayan LCT-type pegmatites","authors":"Yong-Neng Zhao, Jun-Xing Zhao, Noreen J. Evans, Chang-Tong He, Rui-Zhe Shi, Shen Gao, Li-Qun Zhu, Ke-Zhang Qin, Ming-Jian Cao","doi":"10.1007/s00126-025-01424-1","DOIUrl":"https://doi.org/10.1007/s00126-025-01424-1","url":null,"abstract":"","PeriodicalId":18682,"journal":{"name":"Mineralium Deposita","volume":"57 1","pages":""},"PeriodicalIF":4.8,"publicationDate":"2026-01-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145947202","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Geochemistry and Li isotopes of micas: implications for granitic magma evolution and fluid exsolution at the Laiziling Sn-polymetallic deposit in southern Hunan Province (South China) 湘南来子岭锡多金属矿床云母地球化学及Li同位素特征:花岗岩岩浆演化及流体溶蚀意义
IF 4.8 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-05 DOI: 10.1007/s00126-025-01425-0
Kaixuan Li, Sheng Huang, Cheng-Biao Leng, Ruyi Zhao, Dazhao Wang, Xianping Luo
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引用次数: 0
Fe-oxyhydroxide deposits at Semenov hydrothermal field (13°30'N), Mid-Atlantic ridge: insights into formation, modification and resource potential. 中大西洋海岭Semenov热液田(13°30′n)铁氧氢氧化铁矿床:成因、改造和资源潜力
IF 4.9 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-01 Epub Date: 2025-08-01 DOI: 10.1007/s00126-025-01376-6
Christian S Bishop, Anna Lichtschlag, Stephen Roberts, Maxime Lesage, Bramley J Murton

Secondary Fe-oxyhydroxide (FeOOH) forms at seafloor massive sulphide (SMS) deposits through the oxidation of sulphide minerals by oxygenated seawater. Secondary FeOOH deposits are enriched in economically important metals, such as Cu and Zn, potentially representing an additional resource. However, how the metal content of secondary FeOOH evolves through post-formational modification at the seafloor, is poorly understood. Moreover, FeOOH can form as metal-poor primary precipitates, but our knowledge is insufficient to effectively discriminate between primary and secondary FeOOH at SMS deposits. At the Mid-Atlantic Ridge hosted Semenov hydrothermal field, primary FeOOH deposits are typically metal-depleted (< 0.4 wt% Cu + Ni + Zn, n = 6) and form layered chimney structures with alternating Mn-oxide and FeOOH bands, with the fluid conduit lined with green smectite. In contrast, secondary FeOOH deposits are enriched in Cu, averaging 2.40 wt% (n = 31), and exhibit diverse textural morphologies including chimney, brecciated, layered, ochre, ocherous and massive, inherited from the sulphide protolith. Secondary FeOOH behaves similarly to terrestrial gossans, acting as a metal trap through sorption or precipitation of metals released during underlying sulphide oxidation. A correlation between the Cu content of secondary FeOOH and that of sulphide suggests its potential use as a geochemical vector in exploration. Finally, the Cu content in the secondary FeOOH remains stable even under prolonged exposure to seawater at the seafloor, indicating that older, off-axis, buried and oxidised SMS deposits may still contain secondary FeOOH with appreciable amounts of Cu. Overall this study demonstrates the potential of secondary FeOOH as a potential metal resource and a tool to guide exploration at SMS deposits.

Supplementary information: The online version contains supplementary material available at 10.1007/s00126-025-01376-6.

次级氢氧化铁(FeOOH)在海底块状硫化物(SMS)沉积物中通过含氧海水对硫化物矿物的氧化形成。次生FeOOH矿床富含经济上重要的金属,如Cu和Zn,可能是一种额外的资源。然而,次生FeOOH的金属含量是如何通过海底地层改造而演变的,人们知之甚少。此外,FeOOH可以形成贫金属的原生沉淀,但我们的知识不足以有效区分SMS矿床的原生和次生FeOOH。在大西洋中脊的Semenov热液区,原生FeOOH矿床通常是金属枯竭(n = 6),形成层状烟囱结构,mn -氧化物和FeOOH条带交替存在,流体导管内衬绿色蒙脱石。次生FeOOH矿床富集Cu,平均富集量为2.40 wt% (n = 31),呈现出烟囱状、角砾岩状、层状、赭石状、赭石状和块状等多种结构形态,继承自硫化物原岩。次生FeOOH的行为类似于陆地上的蛛丝,通过吸附或沉淀在潜在硫化物氧化过程中释放的金属,起到金属捕集器的作用。次级FeOOH的Cu含量与硫化物的Cu含量之间的相关性表明其在勘探中可能作为地球化学矢量。最后,即使长时间暴露在海底海水中,次级FeOOH中的Cu含量也保持稳定,这表明较老的、离轴的、埋藏的和氧化的SMS沉积物可能仍然含有含有相当数量Cu的次级FeOOH。总的来说,这项研究表明了次生FeOOH作为一种潜在的金属资源和指导SMS矿床勘探的工具的潜力。补充信息:在线版本包含补充资料,可在10.1007/s00126-025-01376-6获得。
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引用次数: 0
Germanium enrichment in coal-hosted germanium deposits: evidence from in-situ sulfur and iron isotopes of pyrite in the Wulantuga germanium deposit, Inner Mongolia, China 煤型锗矿床中的锗富集:内蒙古乌兰图格锗矿床黄铁矿原位硫和铁同位素证据
IF 4.8 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2025-12-27 DOI: 10.1007/s00126-025-01420-5
Yan Gao, Victor P. Nechaev, James C. Hower, Jingjing Liu, Wenhua Li, Shifeng Dai, Zhengfu Zhao, Mengda Yao, Hao Li
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引用次数: 0
Tracing fluid evolution forming multistage wolframite mineralization in vein-type tungsten (-tin) deposit: new insight from LA-ICP-MS analysis of fluid inclusion 脉状钨(锡)矿床中形成多阶段黑钨矿化的流体演化:LA-ICP-MS流体包裹体分析的新见解
IF 4.8 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2025-12-23 DOI: 10.1007/s00126-025-01419-y
Zhi-Lin Cheng, Jun-Yi Pan, Pei Ni, Li-Li Chen, Jian-Ming Cui, Zhe Chi, Jun-Ying Ding
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引用次数: 0
Coupling whole-rock geochemistry with trace elements and S-isotope analyses of pyrite to unravel distinct precipitation processes responsible for the Yaouré gold deposit formation (Côte d’Ivoire, West Africa) 黄铁矿的全岩地球化学与微量元素和s同位素分析相结合,揭示yaour<s:1>金矿床形成的不同降水过程(Côte d 'Ivoire,西非)
IF 4.8 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2025-12-19 DOI: 10.1007/s00126-025-01415-2
Nicolas Mériaud, Nicolas Thébaud, Quentin Masurel, Steffen Hagemann, Laure A.J. Martin, Leonid Danyushevsky, Paul Olin
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引用次数: 0
Controls of Early Jurassic Paleo-Pacific plate subduction on tectono-mineralization in the eastern Central Asian Orogenic Belt: evidence from copper and gold mineralization 中亚造山带东部早侏罗世古太平洋板块俯冲对构造成矿作用的控制:来自铜、金成矿作用的证据
IF 4.8 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2025-12-15 DOI: 10.1007/s00126-025-01411-6
Weipeng Liu, Xiaohui Zeng, Bizheng Yang, Xinran Ni, Xingmin Zhang, Zhendong Tian, Changzhou Deng
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引用次数: 0
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Mineralium Deposita
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