Extraction of ore components from mafic magmas by immiscible carbonate and salt melts: evidence from melt and fluid inclusions in minerals

被引：0
|
作者：
Solovova, IP [1 ]
Girnis, AV [1 ]
机构：
[1] Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow, Russia
来源：
MINERAL EXPLORATION AND SUSTAINABLE DEVELOPMENT, VOLS 1 AND 2 | 2003年
关键词：
melt inclusion; alkali basaltoid; carbonatite; liquid immiscibility; fluid;
D O I：
暂无
中图分类号：
P57 [矿物学];
学科分类号：
070901 ;
摘要：
Melt and fluid inclusions were studied in minerals of two alkaline igneous complexes, Verkhnedunkeldykskii massif in the eastern Pamirs and Gardiner massif in East Greenland. Minerals of the Verkhnedunkeldykskii massif contain silicate and salt (phosphate-sulfate-carbonate) melt inclusions. The early immiscible carbonatitic melts were formed at temperatures higher than 1000degreesC, and phosphate-fluoride-chloride melts were trapped at 740-570degreesC. With decreasing temperature, the salt melts evolved into highly saline hydrothermal solutions. Melilite from the melilitolite of the Gardiner complex contain cogenetic silicate and carbonate melt inclusions, which were trapped at 1060-900degreesC. Crystallization of high-temperature carbonate and salt melts in inclusions gave rise to a variety of minerals including those enriched in trace elements (REE, Ba, Sr).
引用
收藏
页码：635 / 637
页数：3
相关论文
共 50 条
  • [1] The transition from peraluminous to peralkaline granitic melts:: Evidence from melt inclusions and accessory minerals
    Thomas, R.
    Webster, J. D.
    Rhede, D.
    Seifert, W.
    Rickers, K.
    Foerster, H. -J.
    Heinrich, W.
    Davidson, P.
    [J]. LITHOS, 2006, 91 (1-4) : 137 - 149
  • [2] Melts and fluids in natural mineral and ore formation: modern studies of fluid and melt inclusions in minerals
    Smirnov, S. Z.
    Sharygin, V. V.
    Szabo, Cs
    [J]. RUSSIAN GEOLOGY AND GEOPHYSICS, 2011, 52 (11) : 1283 - 1285
  • [3] Fluid overpressure in andesite melts from Central Slovakia: Evidence from inclusions in minerals
    Naumov, VB
    Tolstykh, ML
    Kovalenker, VA
    Kononkova, NN
    [J]. PETROLOGY, 1996, 4 (03) : 265 - 276
  • [4] Multiphase carbonate-salt immiscibility in carbonatite melts: data on melt inclusions from the Krestovskiy massif minerals (Polar Siberia)
    L. I. Panina
    [J]. Contributions to Mineralogy and Petrology, 2005, 150 : 19 - 36
  • [5] Multiphase carbonate-salt immiscibility in carbonatite melts: data on melt inclusions from the Krestovskiy massif minerals (Polar Siberia)
    Panina, LI
    [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 2005, 150 (01) : 19 - 36
  • [6] Inclusions of immiscible sulfide melts in olivine phenocrysts from mantle-derived magmas
    McNeill, A. W.
    Danyushevsky, L. V.
    Kamenetsky, V.
    Feig, S.
    Crawford, At
    [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 2008, 72 (12) : A616 - A616
  • [7] Alkalis in carbonatite magmas: New evidence from melt inclusions
    Sokolov, SV
    Veksler, IV
    Senin, VG
    [J]. PETROLOGY, 1999, 7 (06) : 602 - 609
  • [8] Silicate and salt melts in the genesis of the industrial'noe tin deposit: Evidence from inclusions in minerals
    Naumov, V. B.
    Kamenetsky, V. S.
    [J]. GEOCHEMISTRY INTERNATIONAL, 2006, 44 (12) : 1181 - 1190
  • [9] Silicate and salt melts in the genesis of the industrial’noe tin deposit: Evidence from inclusions in minerals
    V. B. Naumov
    V. S. Kamenetsky
    [J]. Geochemistry International, 2006, 44 : 1181 - 1190
  • [10] Fluorine concentration in magmatic melts: Evidence from inclusions in minerals
    Naumov, VB
    Kovalenko, VI
    Dorofeeva, VA
    [J]. GEOKHIMIYA, 1998, (02): : 147 - 157
12345