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Geology of Mongolia

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molybdenum, tungsten, tin, oil, iron, coal, evaporites and fluorite, followed by the activities of the Polish-Mongolian Paleontological Expedition from 1946 to 1949. Mongolneft, a state owned oil company launched in 1948. The Geological Prospecting Survey (renamed Ministry of Geology in 1961) was created in 1957.
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Alexander von Humboldt and N.M. Prewalskii made the first geological reconnaissance of Mongolia. Russian geologists were active prior and after World War I, into the Soviet period, conducting expeditions into the Gobi Desert. The Russian Geological Exploration Expeditions from 1932 to 1937 discovered
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structures seem to control for chromium, titanium and vanadium. Lead, zinc, copper and gold mineralization across all three metallogenic provinces. The Boro ore zone traces the Changajn and Chentejn mountains in the East Mongolian province with gold deposits. Triassic and Jurassic igneous deposits
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Tectonic belts in Mongolia have a strong influence on where base metal ores have formed. The North Mongolian Metallogenic Province is part of the Mongolian Altai Caledonides, with a southern boundary at a deep fault near Bulgan. The East Mongolian Metallogenic Province covers two-thirds of the
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formations experienced rifting from 1.7 to 1.6 billion years ago and again around 800 million years ago. The closing of a late Proterozoic ocean generated the ophiolites and the oldest basement rock. The Baikalides and Altaid mountain belts represent the accretion of island arcs into the
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The Valley of Lakes is the center of Mongolia's extensive coal deposits, which date to the Carboniferous in the west and the Permian in the south. Oil is known from intracratonic basins in the southeast, centered around the Sajnsand oil field.
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had a major impact on the region. Crustal extension created the Mongolian Plateau, while rifting, crustal thinning, block faulting and basalt eruptions produced terrain very similar to the
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hold many of the country's metal resources in the same province. Deep-seated faults host mercury deposits. Northwest of Muren, aluminum deposits are associated with nepheline
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is made up a complicated array of microcontinents and island chains accreted together over the past half billion years, producing varied terrain and tectonics.
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Iron ore forms as metasomatic skarn deposits and together with manganese ore is common in the East Mongolian province. Hercynian and Caledonian
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country and was highly influenced by Mesozoic magmatic activity. The South Mongolian Metallogenic Province is a third grouping.
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Encyclopedia of European & Asian Regional Geology
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Index

Mongolia
structural geology
Paleozoic
Precambrian
Riphean
ophiolite
Paleozoic
Gondwana
Mesozoic
Cenozoic
Basin and Range province
ophiolite
syenite
sillimanite
gneiss
chrysotile
mylonite
malachite
Moores & Fairbridge 1997
Moores & Fairbridge 1997
Moores & Fairbridge 1997
v
t
e
Geology of Asia
Sovereign states
Afghanistan
Armenia
Azerbaijan
Bahrain

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