نتایج جستجو برای: host countrys mineral policies
تعداد نتایج: 399503 فیلتر نتایج به سال:
Sheltered inside crystals, mineral inclusions preserve crucial information on the geological history of our planet. These allow estimation pressure and temperature trajectories metamorphic rocks, but also can tell about rock mineralogy, provenance, geodynamic petrogenetic processes. This is recovered under axiom that have remained immutable objects do not change shape after their entrapment. Co...
ion of Transaction Demarcation in Component-Oriented Platforms Romain Rouvoy and Philippe Merle INRIA Jacquard Project, Laboratoire d’Informatique Fondamentale de Lille, UPRESA 8022 CNRS – U.F.R. I.E.E.A. – Bâtiment M3, Université des Sciences et Technologies de Lille, 59655 Villeneuve d’Ascq Cedex, France, rouvoy, merle @lifl.fr Abstract. Component-oriented middleware becomes the privileged su...
Potato virus X multiplication as influenced by mineral nutritions of host has been studied by some workers (HELMS & POUND 1955, BAWD EN & KASSANIS 1950, GANGULI & al. 1963). They have mostly studied the effect of nitrogen, phosphorus and potassium nutrition on the host growth and virus multiplication. Host nutrition with magnesium in relation to PVX multiplication has not been much studied. The...
The Golgohar iron mine is located about 55 km southwest of Sirjan in the Sanandaj-Sirjan structural zone. We distinguished five mineralization zones, on the bases of mineral assemblage with magnetite. The gangue minerals are pyrite, pyrrhotite, chalcopyrite, siderite, apatite, serpentine, talc, chlorite, amphibole, calcite, dolomite and quartz. All chlorites are tri-octahedral in nature. The ch...
Angouran zinc and lead deposit is located about 135 km west of Zanjan city, in the northwest of the Sanandaj-Sirjan structural zone The results of this study indicate that the dolomitic alteration occurred in the carbonate hanging-wall and the presence of ankerite in the schist footwall. The main host of ore deposit is metamorphic carbonate. The Angouran dolomite is secondary and hydrothermal. ...
Roshtkhar Iron deposit is located in southeast of Khorasan Razavi Province about 48 Km east of Roshtkhar. This deposit is geologically located in the northeast of the Lut block in the Khaf-Bardaskan volcanic- plutonic belt. Intermediate igneous rocks such as stock, dyke, lava and pyroclastic deposits are host rock. Igneous rocks are dioritic porphyry, monzosyenitic porphyry, andesite, basalt an...
Shurchah antimony deposit is located in flysch zone of eastern Iran. The antimony mineralization was formed in silicic veins that hosted by highly silicified and brecciated granitoids and low-grade metamorphic rocks which are rich in phyllosilicate minerals. Stibnite is the most aboundant Sb-bearing ore mineral in the veins and is associated with pyrite, chalcopyrite, arsenopyrite and gold. Sen...
The Great Basin of the Western United States has thin continental crust and geologic structures that have controlled the emplacement of significant precious and base metal mineralization. Many of the mineral deposits in the Great Basin were emplaced by hydrothermal processes that altered the mineralogy of their host rock assemblages and facilitated concentration of metals. In the 1960’s and 197...
Introduction: The presence of sulfates on the surface of Mars was indicated by a strong Mg-S correlation in the fluorescence data obtained by the Viking landers [1]. Sulfates were subsequently identified as being present in the soil at the Pathfinder landing site at a concentration of ~ 10 % MgSO4 [2]. Data from the Opportunity rover indicates that sulfates of probable evaporite origin are pres...
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