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S and Pb Isotope Geochemistry of the carbonate-hosted Au-Ag-Zn ± Pb deposits in the Maden Village (Ulukışla-Niğde), Central Taurides, South Turkey 土耳其中部Taurides Maden Village (Ulukışla-Niğde)碳酸盐岩Au-Ag-Zn±Pb矿床S、Pb同位素地球化学特征
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2019-06-11 DOI: 10.1127/NJMA/2019/0166
Asuman Kahya, E. Kuşcu, O. Cengiz, M. Yıldız
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引用次数: 1
Mineralogy and geochemistry of the Dehshir listvenites, central Iran 伊朗中部德希尔橄榄岩的矿物学和地球化学
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2019-06-01 DOI: 10.1127/NJMA/2019/0091
M. Ahankoub, M. Mackizadeh
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引用次数: 1
Biotite compositional variations – A physicochemical approach to investigate crustal involvement and ore potential in Middle Jurassic plutonic rocks from the Malayer-Boroujerd Plutonic complex, W Iran 黑云母成分变化——用物理化学方法研究伊朗马拉耶-博鲁杰德深部杂岩中侏罗统地壳参与和找矿潜力
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2019-06-01 DOI: 10.1127/NJMA/2019/0131
H. Yeganehfar, R. Deevsalar, Vahid Ahadnejad, R. Shinjo, I. Neill
Biotite is the most frequent ferromagnesian phase in granitoids from the Malayer-Boroujerd Plutonic complex (MBPC), Zagros Orogen. The abundance of biotite decreases from granitoids towards dioritic intrusions, dioritic and gabbroic dykes to gabbroic intrusions coincident with increase in hornblende/biotite ratio. Primary magmatic biotite composition in the MBPC granitoids (Fe-rich type) changes from annite to siderophyllite, while Fe-depleted secondary biotites from the altered gabbros and gabbroic-dioritic dykes approximate to the phlogopite-eastonite series, and those from least-altered gabbros display average composition of these groups, however, extend towards high-Al end-members. Using Ti-in-biotite geothermometer, the crystallization temperature varies between 550 °C to 750 °C in MBPC granitoids (P 10–15 bars). Mode-III: biotite crystallized at higher oxidizing conditions (f(O2) > 10–10 bars) in gabbroic and dioritic dykes as well as gabbroic intrusions. The progressive decreases in f (O 2)–values and oxidizing conditions from I-type to S-type granites (above HM-to below QFM-buffer) reflect increasing incorporation of less-oxidized upper crustal materials during magmagenesis. In addition, the highest f (O2) in MBPC mafic intrusive rocks is consistent with a modest crustal contamination, if any. There is lack of evidence for porphyry type alteration zoning and subvolcanic porphyritic intrusions associated with porphyry copper system. The small patches of calc-silicate rocks from the NW-MBPC formed in contact with less oxidized and highly fractionated, crustal-derived granular granitoids and are less predisposed to develop Cu-Au mineraliza- tion. However, given the relatively higher f (O2)-values, the Middle Jurassic mafic intrusive rocks originated from the meta- somatised mantle-wedge beneath SaSiZ, appears to be the best candidate for further ore exploration programs in the area.
黑云母是Zagros造山带Malayer Boroujerd Plutonic杂岩(MBPC)花岗岩类中最常见的铁磁相。黑云母的丰度从花岗岩类向闪长质侵入体、闪长质和辉长岩岩脉向辉长岩侵入体递减,同时角闪石/黑云母比例增加。MBPC花岗质岩石(富铁型)中的原生岩浆黑云母成分从annite变为菱铁矿,而蚀变辉长岩和辉长岩-闪长岩脉中的贫铁次生黑云母接近金云母-东长岩系,而那些蚀变最少的辉长岩中的次生黑云母显示出这些组的平均成分,但向高Al端成员延伸。使用黑云母地热计中的Ti,MBPC花岗质岩石的结晶温度在550°C至750°C之间变化(P 10–15 bar)。模式III:辉长岩和闪长岩脉以及辉长岩侵入体中黑云母在较高氧化条件下结晶(f(O2)>10–10 bar)。从I型到S型花岗岩(HM以上到QFM以下缓冲区)f(O2)值和氧化条件的逐渐降低反映了岩浆发生过程中氧化程度较低的上部地壳物质的掺入增加。此外,MBPC镁铁质侵入岩中的最高f(O2)与适度的地壳污染(如果有的话)一致。斑岩型蚀变分带和与斑岩铜系统相关的次火山斑岩侵入体缺乏证据。NW-MBPC中的小块钙硅酸盐岩石与氧化程度较低、分馏程度较高的地壳衍生粒状花岗质岩石接触形成,不太容易形成Cu-Au矿化。然而,考虑到相对较高的f(O2)值,源自SaSiZ下方变躯体化地幔楔的中侏罗世镁铁质侵入岩似乎是该地区进一步找矿计划的最佳候选者。
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引用次数: 1
Ilmenite generations in kimberlite from Banankoro, Guinea Conakry 几内亚科纳克里Banankoro金伯利岩中的钛铁矿世代
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2018-12-18 DOI: 10.1127/NJMA/2018/0096
Jingyao Xu, J. Melgarejo, M. Castillo-Oliver, L. Arqués, J. Santamaria
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引用次数: 1
Post-mining amorphous Cu-Al hydroxyphosphate from West Caradon Mine, Liskeard, UK 英国Liskeard West Caradon矿开采后的无定形羟基磷酸铜铝
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2018-12-18 DOI: 10.1127/NJMA/2018/0105
N. Chukanov, S. Weiss, N. Meisser, I. Pekov, S. Britvin, S. A. Vozchikova, D. I. Belakovskiy, V. Ermolaeva
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引用次数: 0
Anomalies in the depth of the asthenospheric mantle: key to the enigma of adakites in the Urumieh-Dokhtar magmatic arc 软流圈地幔深度异常:解开乌鲁木齐- dokhtar岩浆弧埃达克岩之谜的关键
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2018-12-01 DOI: 10.1127/NJMA/2018/0093
M. Sayari, M. Sharifi
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引用次数: 0
Geochemistry, texture, and mineralogy of the supergene iron oxide deposits from the Binaloud zone, NE Iran 伊朗东北部宾鲁德带浅生氧化铁矿床的地球化学、结构和矿物学
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2018-12-01 DOI: 10.1127/njma//2018/0064
P. N. Tehrani, A. A. Calagari, F. Velasco, I. Yusta
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引用次数: 0
REE geochemical characteristics and fluid inclusion studies of the Bagher-Abad fluorite deposit, Central Iran 伊朗中部Bagher Abad萤石矿床稀土元素地球化学特征和流体包裹体研究
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2018-12-01 DOI: 10.1127/NJMA/2018/0124
M. Azizi, S. Alipour, A. Abedini, H. Bagheri
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引用次数: 9
Uranium-rich pyrochlores from the Ilímaussaq complex, South Greenland 来自南格陵兰岛Ilímaussaq复合体的富铀焦绿石
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2018-12-01 DOI: 10.1127/njma/2018/0114
S. Karup-moller
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引用次数: 1
Sulfides in alkaline and peralkaline rocks: textural appearance and compositional variations 碱性和过碱性岩石中的硫化物:结构外观和成分变化
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2018-08-01 DOI: 10.1127/NJMA/2018/0095
Rainer J. Babiel, M. Marks, U. Neumann, G. Markl
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引用次数: 4
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Neues Jahrbuch Fur Mineralogie-Abhandlungen
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