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They reveal that the chemical composition of the deep mantle has remained almost intact since the Earth's formation 4.5 ...

Photo 2. (left) Evidence for magma mixing just east of the mineralized mafic-ultramafic rock shown in Photo 1 from the Trans Canada Highway exposure, as part of a gradational change from leucocratic ...

Emerging evidence suggests that plate tectonics, or the recycling of Earth's crust, may have begun much earlier than previously thought — and may be a big reason that our planet harbors life.

ABSTRACT: The mafic enclaves from Paleoproterozoic domain are considered to be the results of large-scale crust-mantle interaction and magma mixing. In this paper, petrography, mineralogy and ...

ABSTRACT: The mafic enclaves from Paleoproterozoic domain are considered to be the results of large-scale crust-mantle interaction and magma mixing. In this paper, petrography, mineralogy and ...

"To achieve this, we modelled mixing an impacting planetesimal with the mantle materials in three flowing phases: solid silicate minerals, molten silicate magma and liquid metal," said Dr Jun ...

“To achieve this, we modeled mixing an impacting planetesimal with the mantle materials in three flowing phases: solid silicate minerals, molten silicate magma and liquid metal,” said Dr. Jun Korenaga ...

“To achieve this, we modeled mixing an impacting planetesimal with the mantle materials in three flowing phases: solid silicate minerals, molten silicate magma and liquid metal,” said Dr. Jun ...

“To achieve this, we modeled mixing an impacting planetesimal with the mantle materials in three flowing phases: solid silicate minerals, molten silicate magma and liquid metal,” said Dr. Jun ...

“This is definitely, without a doubt, the largest eruption since Mt. Pinatubo in 1991,” said corresponding author Scruggs, who studies magma mixing and eruption triggering mechanisms, and recently ...