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Hydrothermal cerium oxide in manganese-oxide-cemented breccia, Quadrilátero Ferrífero of Minas Gerais, Brazil 水热氧化铈在氧化锰胶结角砾岩中,Quadrilátero Ferrífero of Minas Gerais,巴西
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2020-07-01 DOI: 10.1127/njma/2020/0184
A. Cabral, F. Rios, L. E. D. Amorim, F. Laufek, L. Graça
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引用次数: 2
Silver minerals in the Unkur sandstone-hosted Cu deposit (Transbaikalia region, Russia) 俄罗斯外贝加尔地区Unkur砂岩型铜矿床中的银矿物
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2020-07-01 DOI: 10.1127/njma/2020/0192
K. Novoselov, E. Belogub, E. Palenova, I. Blinov
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引用次数: 2
Serpentinization and chloritization of metamorphosed lherzolites in Darreh-Deh (east of Nain Ophiolite, Central Iran): Calcium source for rodingitization and tremolitization Darreh-Deh(伊朗中部Nain蛇绿岩以东)变质橄榄岩的蛇纹石化和绿泥石化:岩石化和透石化的钙源
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2020-07-01 DOI: 10.1127/njma/2019/0163
N. Shirdashtzadeh, G. Torabi
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引用次数: 1
Fehrite, MgCu4(SO4)2(OH)6 · 6H2O, the magnesium analogue of ktenasite from the Casualidad mine near Baños de Alhamilla, Almeria, Spain 西班牙Almeria Baños de Alhamilla附近Casualidad矿中钾氧化镁类似物MgCu4(SO4)2(OH)6·6H2O
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2020-01-01 DOI: 10.1127/njma/2020/0218
J. Schlüter, T. Malcherek, B. Mihailova, Christian Rewitzer, R. Hochleitner, D. Müller, A. Günther
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引用次数: 2
Composition of minerals from the skarn deposits Väster Silvberg (Sweden) and Tumurtijn-ovoo (Mongolia): Indications of different element supply in submarine hydrothermal-sedimentary ore genesis 瑞典Väster Silvberg和蒙古Tumurtijn-ovoo夕卡岩矿床矿物组成:海底热液-沉积矿床成因中不同元素供应的指示
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2019-11-18 DOI: 10.1127/njma/2019/0123
W. Gottesmann, B. Gottesmann
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引用次数: 0
Petrogenesis of an alkaline lamprophyre (camptonite) with ocean island basalt (OIB)-affinity at the NW margin of the Cuddapah basin, eastern Dharwar craton, southern India 印度南部Dharwar克拉通东部Cuddapah盆地西北缘与洋岛玄武岩(OIB)亲缘的碱性煌斑岩(camponite)的岩石成因
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2019-11-18 DOI: 10.1127/njma/2019/0179
R. Giri, Praveer Pankaj, N. V. C. Rao, R. Chakrabarti, D. Pandit
We report petrology and geochemistry (including Sr and Nd isotopes) of a fresh lamprophyre at Ankiraopalli area at the north-western margin of Paleo-Mesoproterozoic Cuddapah basin, eastern Dharwar craton, southern India. Ankiraopalli samples possess a typical lamprophyre porphyritic-panidiomorphic texture with phenocrysts of kaersutite and diopside set in a plagioclase dominant groundmass. Combined mineralogy and geochemistry classify it as alkaline lamprophyre in general and camptonite in particular. Contrary to the calc-alkaline and/or shoshonitic orogenic nature portrayed by lamprophyres occurring towards the western margin of the Cuddapah basin, the Ankiraopalli samples display trace element composition revealing striking similarity with those of ocean island basalts, Italian alkaline lamprophyres and highlights an anorogenic character. However, the Sr-87/Sr-86(initial) (0.710316 to 0.720016) and epsilon Nd-initial (-9.54 to -9.61) of the Ankiraopalli lamprophyre show derivation from an `enriched' mantle source showing long term enrichment of incompatible trace elements and contrast from those of (i) OIB, and (ii) nearby Mahbuhnagar alkaline mafic dykes of OIB affinity. Combining results of this study and recent advances made, multiple mantle domains are identified in the Eastern Dharwar craton which generated distinct Mesoproterozoic lamprophyre varieties. These include (i) Domain I, involving sub-continental lithospheric mantle source essentially metasomatized by subduction-derived melts/fluids (represented by orogenic calcalkaline and/or shoshonitic lamprophyres at the Mudigubba, the Udiripikonda and the Kadiri); (ii) Domain II, comprising a mixed sub-continental lithospheric and asthenospheric source (represented by orogenic-anorogenic, alkaline to calc-alkaline transitional lamprophyres at the Korakkodu), and (iii) Domain III, representing a sub-continental lithospheric source with a dominant overprint of an asthenospheric (plume) component (represented by essentially alkaline lamprophyres at the Ankiraopalli). Our study highlights the varied mantle source heterogeneities and complexity of geodynamic processes involved in the Neoarchean-Paleo/Mesoproterozoic evolution of the Eastern Dharwar craton.
本文报道了印度南部Dharwar克拉通东部古-中元古代Cuddapah盆地西北缘Ankiraopalli地区一个新鲜煌斑岩的岩石学和地球化学(包括Sr和Nd同位素)。Ankiraopalli样品具有典型的煌斑岩-斑岩-泛自形结构,在斜长石为主的地块中嵌有凯尔长岩和透辉石的斑晶。结合矿物学和地球化学,将其分类为碱性煌斑岩,特别为喜树斑岩。与Cuddapah盆地西缘煌斑岩的钙碱性和(或)钾玄武岩造山性质相反,Ankiraopalli煌斑岩样品的微量元素组成与洋岛玄武岩、意大利碱性煌斑岩的微量元素组成惊人地相似,具有明显的造山特征。然而,Ankiraopalli煌斑岩的Sr-87/Sr-86(初始值)(0.710316 ~ 0.720016)和epsilon nd -初始值(-9.54 ~ -9.61)显示出源自一个长期富集不相容微量元素的“富集”地幔源,并与(i) OIB和(ii)靠近OIB亲和的Mahbuhnagar碱性基性岩脉形成对比。结合本研究成果和近期研究进展,确定了东达瓦尔克拉通的多个地幔域,形成了独特的中元古代煌斑岩品种。其中包括(i)第一领域,涉及次大陆岩石圈地幔源,主要由俯冲衍生的熔体/流体交代(以Mudigubba、Udiripikonda和Kadiri的造山钙碱性和/或shoshonic煌斑岩为代表);(ii)区域ii,包括一个混合的次大陆岩石圈和软流圈源(以造山-造山、碱性到钙碱性过渡型煌斑岩为代表,位于Korakkodu); (iii)区域iii,代表一个以软流圈(羽流)成分为主的次大陆岩石圈源(主要以Ankiraopalli的碱性煌斑岩为代表)。研究结果揭示了东达尔瓦克拉通新太古代-古/中元古代演化过程中地幔源非均质性的多样性和地球动力学过程的复杂性。
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引用次数: 3
Late-Mesozoic tectonic evolution and magmatic history of the Zhe-Gan-Wan region, SE China: evidence from the Shiling rhyolite and other Yanshanian granitoids 浙赣皖地区晚中生代构造演化与岩浆历史:来自石岭流纹岩和其他燕山期花岗类的证据
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2019-11-01 DOI: 10.1127/njma/2019/0142
Xiu Liu, Xinqi Yu, Pengju Li, Jun Hu, Mengyan Liu, Yan Zeng
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引用次数: 2
The carbonate and silicate mineralogy of the Zhilingtou gold-silver deposit, Zhejiang Province, south-eastern China 浙江直岭头金银矿床碳酸盐和硅酸盐矿物学研究
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2019-11-01 DOI: 10.1127/NJMA/2019/0143
S. Karup-moller, E. Makovicky, L. Jiuling
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引用次数: 0
Green mawbyite, PbFe3+Fe2+0.4Zn0.6(AsO4)2OH(H2O), from the Lagoa mine, northern Portugal 绿色马白石,PbFe3+Fe2+0.4Zn0.6(AsO4)2OH(H2O),产自葡萄牙北部Lagoa矿
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2019-11-01 DOI: 10.1127/NJMA/2019/0167
Pedro Alves, W. Mumme, I. Grey, C. MacRae, R. Gable
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引用次数: 0
The Chargar Au-Cu deposit: an example of low-sulfidation epithermal mineralization from the Tarom subzone, NW Iran Chargar金铜矿床:以伊朗西北部Tarom亚带低硫化浅成热液成矿为例
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2019-06-11 DOI: 10.1127/NJMA/2019/0158
S. H. M. Motlagh, M. Ghaderi
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引用次数: 11
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Neues Jahrbuch Fur Mineralogie-Abhandlungen
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