Steel is a foundation of national economic construction. Magnetite and hematite are the main minerals for the recovery of Fe to make steel. The main source of Fe deposits in most of the world is banded iron formation, but in China magmatic-hydrothermal Fe deposits are the main Fe-enriched (total Fe > 50%) type of deposit.
WhatsApp: +86 18221755073The formation of iron-oxide–apatite (IOA) deposits is much debated. Studies on the origin of IOA deposits have often focused on the δ 18 O values of magnetite, which were suggested to reflect isotopic equilibrium with magmas or with magmatic water; i.e., H 2 O in equilibrium with magma (e.g., Jami et al., 2007; Nyström et al., 2008; Knipping et al., 2015; …
WhatsApp: +86 18221755073The origin of magnetite-(apatite) iron deposits (MtAp) is one of the most contentious issues in ore geology with competing models that range from hydrothermal to magmatic processes.Here we report ...
WhatsApp: +86 182217550731 Magmatic immiscibility and the origin of magnetite-(apatite) iron deposits 2 3 Dorota K. Pietruszka 1, John M. Hanchar 1*, Fernando Tornos 1,2, Richard Wirth 3, Nathan A.
WhatsApp: +86 18221755073The origin of magnetite-(apatite) iron deposits (MtAp) is among the most contentious issue in ore geology with competing models involving purely hydrothermal to magmatic processes.
WhatsApp: +86 18221755073Iron oxide–apatite deposits can form from purely igneous (~1,000–800 °C), through late magmatic or magmatic–hydrothermal (~800–600 °C), to purely hydrothermal …
WhatsApp: +86 18221755073Iron oxide–apatite deposits, including the massive deposits at Kiruna, Sweden (Fig. 1), are principally comprised of magnetite and apatite minerals.Models for their formation …
WhatsApp: +86 18221755073Abstract. This descriptive model for magmatic iron-titanium-oxide (Fe-Ti-oxide) deposits hosted by Proterozoic age massif-type anorthosite and related rock types presents their geological, mineralogical, geochemical, and geoenvironmental attributes.
WhatsApp: +86 18221755073Magmatic ore deposits are masses of igneous rock enriched in useful chemical elements to such an extent that it is feasible to mine them at a profit. To be considered an ore, an accumula- ... With the sole exception of iron, the ore elements identified in Figure 2are all trace elements in primary magmas, and their
WhatsApp: +86 18221755073Magnetite δ 18 O values from the Zhibo and Chagangnuoer deposits compared to other volcanic-hosted, magmatic iron-oxide deposits (modified after Jonsson et al., 2013). The diagram shows magnetites in equilibrium with MORB (green field) and the range for typical 'ortho-magmatic' magnetites after Taylor (1967) – (blue field).
WhatsApp: +86 182217550731. Introduction. Magnetite is a common oxide mineral in igneous, metamorphic, and sedimentary rocks. They also widely occur in a variety of iron ores, including BIF (banded iron formation), Kiruna-type, magmatic Fe Ti oxide, and iron skarn deposits (Dupuis and Beaudoin, 2011, Huberty et al., 2012, Nadoll et al., 2012), as well as in other types of hydrothermal …
WhatsApp: +86 182217550731. Introduction. China has a rich reserve of iron ores, and hosts most of the major types of iron deposits recognized over the world. However, most of these deposits are low-grade ores (<50% Fe), and the high-grade iron ores only account for ∼1% of the total iron ore resources (Zhang et al., 2014a).During 50s to 70s of the last century, two major research and …
WhatsApp: +86 18221755073Further, our model explains the observed coexisting purely magmatic and hydrothermal-magmatic features and allows a genetic connection between Kiruna-type IOA and iron oxide–copper–gold deposits, contributing to a …
WhatsApp: +86 18221755073The origin of magnetite-(apatite) iron deposits (MtAp) is one of the most contentious issues in ore geology with competing models that range from hydrothermal to magmatic processes. Here we report ...
WhatsApp: +86 182217550739.3.1.1 Magmatic Sulfides and Cumulates. Mafic and ultramafic magmas, like all common magmas, contain the major elements oxygen, silicon, aluminum, iron, calcium, sodium, potassium, and magnesium. But they …
WhatsApp: +86 1822175507313.8.1 Introduction. Magmatic ore deposits are masses of igneous rock enriched in useful chemical elements to such an extent that it is feasible to mine them at a profit. To be …
WhatsApp: +86 18221755073Porphyry deposits form at several kilometres depth in the crust and are associated with pipe- or dyke-like magmatic intrusions 11,12,13,14,15,19,20,21,22 (see Supplementary Information).These ...
WhatsApp: +86 18221755073Further, our model explains the observed coexisting purely magmatic and hydrothermal-magmatic features and allows a genetic connection between Kiruna-type IOA …
WhatsApp: +86 18221755073The origin of magnetite-(apatite) iron deposits (MtAp) is one of the most contentious issues in ore geology with competing models that range from hydrothermal to magmatic processes. Here we report melt inclusions trapped in plagioclase phenocrysts in andesite hosting the MtAp mineralization at El La …
WhatsApp: +86 18221755073Iron oxide–apatite deposits, including the massive deposits at Kiruna, Sweden (Fig. 1), are principally comprised of magnetite and apatite minerals.Models for their formation range from purely ...
WhatsApp: +86 1822175507390 3 Magmatic (Orthomagmatic) Deposits … 3.1 Introduction Magmatic deposits: ores formed by direct crystallization and accumulation from a magma Deposits associated with mafic–ultramafic rocks • Chromite deposits: (i) stratiform chromite in layered intrusions, and (ii) podiform chromite in ophiolite complexes • Magmatic sulfides (Cu ...
WhatsApp: +86 18221755073The magmatic Fe–Ti–(V) type of iron deposits is hosted in mafic–ultramafic intrusions, and is typified by the Panzhihua-subtype deposits in Hercynian gabbro and the Damiao-subtype deposits in Proterozoic anorthosite complexes. The major ore mineral is Ti–V magnetite. This deposit type accounts for 12.1% of the iron reserves of China ...
WhatsApp: +86 18221755073A Deposit Model for Magmatic Iron-Titanium-Oxide Deposits . Related to Proterozoic Massif Anorthosite Plutonic Suites. U.S. Department of the Interior U.S. Geological Survey. Scientific Investigations Report 2013–5091. COVER. McIntyre mine located in the Adirondack State Park, New York (photo taken by Laurel
WhatsApp: +86 18221755073The predominant types of high-grade iron deposits in China include skarn, sedimentary metamorphic (banded iron-formation, BIF-type), continental/submarine volcanic-hosted and magmatic Fe-Ti-V oxide deposits. Based on a comprehensive review of current studies on these deposits, this paper suggests that the oxygen concentration in atmosphere …
WhatsApp: +86 18221755073This descriptive model for magmatic iron-titanium-oxide (Fe-Ti-oxide) deposits hosted by Proterozoic age massif-type anorthosite and related rock types presents their geological, mineralogical, geochemical, and geoenvironmental attributes. Although these Proterozoic rocks are found worldwide, the majority of known deposits are found within …
WhatsApp: +86 18221755073The origin of magnetite-(apatite) iron deposits (MtAp) is one of the most contentious issues in ore geology with competing models that range from hydrothermal to magmatic processes. Here we report melt inclusions trapped in plagioclase phenocrysts in andesite hosting the MtAp mineralization at El Laco, Chile. The results of our study reveal that …
WhatsApp: +86 18221755073Ore Deposit Geology - July 2013. Magmatic ore deposits, also known as orthomagmatic ore deposits, are deposits within igneous rocks or along their contacts in which ore minerals crystallised from a melt or were transported in a melt. Ore deposits that form in and around igneous rock units as a result of mineral precipitation from aqueous solutions or hydrothermal …
WhatsApp: +86 18221755073The description of magmatic deposits can be carried out according to the host rock association or related to the commodity. The latter is easier and allows to summarize the main groups of deposits present in the Earth's crust from a magmatic viewpoint. ... (VMS) deposits, (3) sedimentary exhalative (SEDEX) deposits, (4) iron oxide-copper-gold ...
WhatsApp: +86 18221755073The origin of magnetite-(apatite) iron deposits (MtAp) is one of the most contentious issues in ore geology with competing models that range from hydrothermal to magmatic processes.
WhatsApp: +86 18221755073Porphyry Cu ± Mo ± Au deposits (porphyry) and iron oxide copper-gold deposits formed by magmatic-hydrothermal systems (MH-IOCG) share many features, most notably enrichments in Fe, Cu, and Au, as well as an association with calc-alkaline to mildly alkaline magmas generated in orogenic (subduction to collision) and postorogenic tectonic settings.
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