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Waipouaite, Ca3(V4+4.5V5+ 0.5)O9[(Si2O5(OH)2][Si3O7.5(OH)1.5]·11H2O, a new polyoxovanadate mineral from the Aranga Quarry, New Zealand Waipouaite, Ca3(V4+4.5V5+ 0.5)O9[(Si2O5(OH)2][Si3O7.5(OH)1.5]·11H2O,产于新西兰Aranga采石场
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-08-01 DOI: 10.2138/am-2023-9048
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引用次数: 0
Characterizing Basalt-Atmosphere Interactions on Venus: A Review of Thermodynamic and Experimental Results 金星上玄武岩-大气相互作用的表征:热力学和实验结果综述
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-08-01 DOI: 10.2138/am-2023-9015
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引用次数: 0
Don Juan Basin, Antarctica: A Chemically-Altering Environment with Martian Analog Potential 南极洲的唐璜盆地:一个具有火星模拟电位的化学改变环境
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-08-01 DOI: 10.2138/am-2022-8779
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引用次数: 0
Scandio-winchite, ideally □(NaCa)(Mg4Sc)(Si8O22)(OH)2, the first Sc-dominant amphibole supergroup mineral from Jordanów Śląski, Lower Silesia, southwestern Poland: description and crystal structure 斯堪的纳维亚□(NaCa)(Mg4Sc)(Si8O22)(OH)2,来自波兰西南部下西里西亚Jordanówšlński的第一种Sc优势角闪石超族矿物:描述和晶体结构
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-08-01 DOI: 10.2138/am-2023-8974
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引用次数: 0
Correlation between Si-Al disorder and hydrogen-bonding distance variation in ussingite (Na2AlSi3O8OH) revealed by one- and two-dimensional multi-nuclear NMR and first-principles calculation 单、二维多核核磁共振和第一性原理计算揭示了乌钢(Na2AlSi3O8OH)中Si-Al无序与氢键距离变化的关系
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-08-01 DOI: 10.2138/am-2023-9008
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引用次数: 0
Tourmaline Growth in the Border and Wall Zones of the Emmons Pegmatite (Maine, Usa): Evidence for Disequilibrium Crystallization and Boundary Layer Formation 埃蒙斯伟晶岩(美国缅因州)边界和壁带中电气石的生长:不平衡结晶和边界层形成的证据
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-08-01 DOI: 10.2138/am-2023-8991
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引用次数: 0
Multi-scale and multi-modal imaging study of mantle xenoliths and petrological implications 地幔捕虏体多尺度多模态成像研究及其岩石学意义
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-08-01 DOI: 10.2138/am-2022-8866
M. Venier, L. Ziberna, G. Roncoroni, A. Demin
22 The accurate textural characterization of mantle xenoliths is one of the fundamental steps to 23 understanding the main processes occurring in the upper mantle, such as sub-solidus 24 recrystallization, magmatic crystallization and metasomatism. Texture, composition, and 25 mineralogy reflect the temperature, pressure, stress conditions, melting and/or contamination events 26 undergone before and during the entrapment in the host magma. For these reasons, characterizing 27 the three-dimensional (3D) texture of silicate, oxide, sulfide and glass phases has great importance 28 in the study of mantle xenoliths. We performed a multi-scale and multi-modal 3D textural analysis 29 based on X-ray computed microtomography (μ-CT) data of three mantle xenoliths from different 30 geodynamic settings (i.e. mobile belt zone, pericraton, oceanic hotspot). The samples were selected 31 to represent different, variably complex, internal structures, composed of grains of different phases, 32 fractures, voids and fluid inclusions of different sizes. We used an approach structured in increasing 33 steps of spatial and contrast resolution, starting with in-house X-ray μ-CT imaging (working at 34 spatial resolution from 30 μm down to 6.25 μm) and moving to high-resolution synchrotron X-ray 35 μ-CT at the micron scale. 36 We performed a 3D characterization of mantle xenoliths comparing the results with the analysis of 37 conventional 2D images (thin sections) obtained by optical microscopy and simulating the random 38
地幔捕虏体的准确结构特征是理解上地幔发生的主要过程(如亚固体重结晶、岩浆结晶和交代)的基本步骤之一。结构、成分和矿物学反映了在宿主岩浆圈闭之前和期间所经历的温度、压力、应力条件、熔融和/或污染事件26。因此,表征硅酸盐、氧化物、硫化物和玻璃相的三维结构在地幔捕虏体研究中具有重要意义。基于来自不同地球动力学背景(活动带、地壳、海洋热点)的3个地幔捕虏体的x射线计算机微断层扫描(μ-CT)数据,进行了多尺度、多模态的三维结构分析。选取31个样品,代表不同的、复杂的内部结构,由不同相的晶粒组成,32个不同大小的裂缝、空隙和流体包裹体。我们采用了一种提高空间和对比度分辨率33个步骤的方法,从内部x射线μ-CT成像(在34空间分辨率下从30 μm下降到6.25 μm)到高分辨率同步加速器x射线35 μ-CT在微米尺度上。我们对地幔捕虏体进行了三维表征,并将结果与光学显微镜获得的37张常规2D图像(薄片)的分析结果进行了比较,并模拟了随机的38张
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引用次数: 0
Single-Crystal X-ray Diffraction on the Structure of (Al,Fe)-bearing Bridgmanite in the Lower Mantle 下地幔含(Al,Fe)桥辉石结构的单晶x射线衍射研究
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-08-01 DOI: 10.2138/am-2023-8969
S. Fu, S. Chariton, Yanyao Zhang, T. Okuchi, V. Prakapenka, Jung‐Fu Lin
12 Here we have performed single-crystal X-ray diffraction (SCXRD) experiments on two high-13 quality crystal platelets of (Al,Fe)-bearing bridgmanite 14 (Mg 0.88 Fe 3+0.065 Fe 2+0.035 Al 0.03 )(Al 0.11 Si 0.90 )O 3 (Fe10-Al14-Bgm) up to 64.6(6) GPa at room 15 temperature in a Boehler-Almax type diamond anvil cell. Refinements on the collected SCXRD 16 patterns reveal reliable structural information of single-crystal Fe10-Al14-Bgm, including unit-17 cell parameters, atomic coordinates, and anisotropic displacement parameters. Together with 18 Mössbauer and electron microprobe analyses, our best single-crystal refinement model indicates 19 that our sample contains ~6.5 mol% Fe 3+ , 3.5 mol% Fe 2+ , and 3 mol% Al 3+ in the large pseudo-20 dodecahedral site (A site), and ~11 mol% Al 3+ in the small octahedral site (B site). This may 21 indicate that Al 3+ in bridgmanite preferentially occupies the B site. Our results show
在这里,我们在boeler - almax型金刚石砧池中对两个高质量的(Al,Fe)含桥菱石14 (Mg 0.88 Fe 3+0.065 Fe 2+0.035 Al 0.03)(Al 0.11 Si 0.90)O 3 (Fe10-Al14-Bgm)晶体片进行了单晶x射线衍射(SCXRD)实验,室温为64.6(6)GPa。对收集到的SCXRD - 16图谱进行细化,得到了单晶Fe10-Al14-Bgm的可靠结构信息,包括单元-17胞参数、原子坐标和各向异性位移参数。结合Mössbauer和电子探针分析,我们的最佳单晶精化模型表明我们的样品在大的伪十二面体位点(A位)含有~6.5 mol% fe3 +, 3.5 mol% fe2 +和3 mol% Al 3+,在小的八面体位点(B位)含有~11 mol% Al 3+。这可能表明铝3+在桥菱石中优先占据B位。我们的结果显示
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引用次数: 0
Geochemical discrimination of pyrite in diverse ore deposit types through statistical analysis and machine learning techniques 基于统计分析和机器学习技术的不同矿床类型黄铁矿地球化学识别
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-08-01 DOI: 10.2138/am-2023-8976
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引用次数: 0
Memorial of Maryellen Cameron (1943−2022) Maryellen Cameron纪念馆(1943−2022)
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-07-27 DOI: 10.2138/am-2023-M1017
Kevin D. Crowle, W. Bagby, John M. Hughes
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引用次数: 0
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