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New Mineral Names 新的矿物名称
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-07-27 DOI: 10.2138/am-2023-NMN10885
A. Celestian
Abstract This issue of New Mineral Names provides a summary of the newly described minerals donowensite, mikehowardite, bortolanite, fluorsigaiite, alumolukrahnite, ferro-ferri-katophorite, tomsquarryite, and argentotetrahedrite-(Zn).
摘要本期《新矿物名称》提供了最新描述的矿物Donowenite、mikehowardite、bortolanite、萤石、铝榴石、铁-铁-钾铁矿、tomsquaryite和银四面体-(Zn)的摘要。
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引用次数: 0
The effect of elemental diffusion on the application of olivine-composition-based magmatic thermometry, oxybarometry, and hygrometry: A case study of olivine phenocrysts from the Jiagedaqi basalts, northeast China 元素扩散对基于橄榄石成分的岩浆测温、氧压和湿法应用的影响——以中国东北嘉格达奇玄武岩橄榄石斑晶为例
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-07-27 DOI: 10.2138/am-2022-8567
Le Zhang, L. Hong, Shengping Qian, Pengli He, Miaohong He, Ya-Nan Yang, Jin-Tuan Wang, Yanqiang Zhang, Zhong‐Yuan Ren
Abstract Olivine compositions are widely used to constrain magmatic thermodynamic conditions such as magmatic temperature, oxygen fugacity, and H2O content. However, elemental diffusion may change the initial compositions and lead to large uncertainty on the estimation of these thermodynamic conditions. In this study, we conducted LA-ICP-MS elemental mapping and EPMA analysis of olivine phenocrysts and olivine-hosted spinel from the Jiagedaqi (JGD) alkaline basalts in northeast China to evaluate the influence of elemental difusion on olivine-composition-based geothermometry, oxybarometry, and hygrometry. The JGD olivines show normal Fo [Mg/(Mg + Fe) × 100 in moles] zoning, with cores having Fo of 77–87 and rims having Fo of 67–73. The constant P contents from core to rim indicate that these compositional zonings were caused mainly by difusion. Because Al is a slow-diffusing element and its content is relatively constant from core to rim, the temperature calculated by the Al-in-olivine thermometer is not influenced by elemental difusion and preserves the JGD olivine crystallization temperature up to 1150 °C. The temperatures calculated using the Sc/Y-in-olivine thermometer, the oxygen fugacity calculated using the olivine–spinel oxybarometer, and the H2O content calculated on the basis of Ca partitioning between olivine and melt are strongly influenced by the diffusion of Fo, Sc/Y, and Ca. However, the compositional plateaus in olivine cores, which were not influenced by elemental diffusion, preserve the magmatic temperature (1150 °C), oxygen fugacity (QFM+1.4), and H2O content (4 wt%) that applied during the formation of the JGD olivines. Together, these findings suggest that the mantle source of the JGD basalts was metasomatized by fluids released from the subducted slab. This study highlights that elemental difusion in olivine phenocrysts can strongly afect the application of olivine-composition-based geothermometers, oxybarometers, and hygrometers. However, primitive olivine cores that have not been influenced by difusion preserve the initial magmatic thermodynamic conditions.
橄榄石组成被广泛用于约束岩浆热力学条件,如岩浆温度、氧逸度和H2O含量。然而,元素扩散可能会改变初始组成,并导致这些热力学条件的估计有很大的不确定性。本文采用LA-ICP-MS元素填图和EPMA分析方法对中国东北嘉格达旗碱性玄武岩中的橄榄石斑晶和含橄榄石尖晶石进行了分析,以评价元素扩散对基于橄榄石组成的测温、测氧和测湿的影响。JGD橄榄石呈正常的Fo [Mg/(Mg + Fe) × 100摩尔分带],岩心Fo值为77 ~ 87,边缘Fo值为67 ~ 73。从岩心到岩缘P含量恒定,表明这些成分分带主要是由扩散引起的。由于Al是一种缓慢扩散的元素,其含量从核心到边缘相对恒定,因此Al-in-橄榄石温度计计算的温度不受元素扩散的影响,并保持JGD橄榄石结晶温度高达1150℃。用Sc/Y-in-橄榄石温度计计算的温度,用橄榄石-尖晶石氧气压表计算的氧逸度,以及根据橄榄石与熔体之间的Ca分配计算的H2O含量都受到Fo、Sc/Y和Ca扩散的强烈影响。然而,橄榄石岩心中的成分高原不受元素扩散的影响,保持了岩浆温度(1150℃)、氧逸度(QFM+1.4)、在JGD橄榄石形成过程中施加的水含量(4wt %)。综上所述,这些发现表明,JGD玄武岩的地幔源是由俯冲板块释放的流体交代的。该研究强调,橄榄石斑晶中的元素扩散会强烈影响基于橄榄石成分的地温计、氧压计和湿度计的应用。原始橄榄石岩心未受扩散影响,保留了岩浆的初始热力条件。
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引用次数: 0
Interfacial Interactions Controlling Adsorption of Metal Cations onto Montmorillonites 界面相互作用控制金属阳离子在蒙脱石上的吸附
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-07-01 DOI: 10.2138/am-2022-8834
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引用次数: 0
Equilibrium Sn isotope fractionation between aqueous Sn and Sn-bearing minerals: Constrained by first-principles calculations 含水锡和含锡矿物之间的平衡锡同位素分馏:受第一性原理计算的约束
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-07-01 DOI: 10.2138/am-2022-8804
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引用次数: 0
The composition of mackinawite mackinawite的成分
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-07-01 DOI: 10.2138/am-2023-8943
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引用次数: 0
Pressure-1 induced phase transitions in Ni-bearing ferrosilite (Ni-En31Fs65) 含镍铁硅岩(Ni-En31Fs65)中压力-1诱导的相变
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-07-01 DOI: 10.2138/am-2022-8879
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引用次数: 0
Scheelite composition fingerprints pulsed flow of magmatic fluid in the Fujiashan W skarn deposit, eastern China 富家山西夕卡岩矿床岩浆流体脉冲流动的白钨矿成分指纹图谱
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-07-01 DOI: 10.2138/am-2022-8917
Yunhao Ji, Guiqing Xie, R. Romer, Wei Li, Qiaoqiao Zhu, Bin Fu
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引用次数: 1
Thermal and combined high-temperature and high-pressure behavior of a natural intermediate scapolite 天然中间石的热及高温高压联合特性
3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-07-01 DOI: 10.2138/am-2023-8962
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引用次数: 0
Using pyrite composition to track the multi-stage fluids superimposed on a porphyry Cu system 利用黄铁矿成分追踪叠加在斑岩铜系统上的多级流体
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-07-01 DOI: 10.2138/am-2022-8727
C. Wua, David R. Cookec, Michael J. Bakerc, Lejun Zhangc, Pei Liangf, Paul Olind, L. Danyushevsky, Huayong Chena
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引用次数: 0
Revisiting the genesis of the adakite-like granitoids in collisional zones: water-fluxed melting of intermediate to felsic rocks with dilution by low Sr/Y phases 碰撞带埃达克岩类花岗岩的成因再探:低Sr/Y相稀释的中长英质岩石的水溶熔融
IF 3.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-07-01 DOI: 10.2138/am-2022-8873
Yuan-Hui Xie, J. Schwartz, Xiao-Wei Li, Keda Cai, Bader Thomas, Huan, Li, Fang-Yue Wang, Xiao-bing Zhang, X. Mo, Guo-Chen Dong
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引用次数: 1
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