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Geochemical data indicate a tholeiitic basalt composition with low Mg O (4–7 wt%) within-plate character based on trace element classification diagrams and source between E-MORB and OIB with only minor contamination from crust or metasomatized lithospheric mantle.Two subgroups are distinguished: Group 1 has gently sloping LREE ((La/Sm) (2.7 wt%), and is transitional from tholeiitic to weakly alkaline in composition.With an area of 6,592,800 square miles (17,075,400 square kilometers), Russia is by far the largest country in the world, covering almost twice the total area of the next-largest country, Canada, and has significant mineral and energy resources.Most of the land consists of broad plain with low hills west of Urals, and vast plains in Siberia.It is also close to the United States (the state of Alaska), Sweden, and Japan across relatively small stretches of water (the Bering Strait, the Baltic Sea, and La Pérouse Strait, respectively).Russia has an extensive coastline of over 23,000 miles (37,000 kilometers) along the Arctic and Pacific Oceans, as well as the Baltic, Black and Caspian seas.
With access to three of the world's oceans -—the Atlantic, Arctic, and Pacific—- Russian fishing fleets are a major contributor to the economy.
The more central Ural Mountains, a north-south range that form the primary divide between Europe and Asia, are also notable.
The lowest point is the Caspian Sea, at 28 meters below sea level.
The Russian Federation emerged as a great power in the early twenty-first century, also considered to be an energy superpower.
The country is considered the Soviet Union's successor state in diplomatic matters, and is a permanent member of the United Nations Security Council.
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The slight differences in REE slopes are consistent with Group 2 on average melting at deeper levels.