Sentence examples for mantle during the from inspiring English sources

The morphological geochemical and mineralogical characteristics of the pocket fills, were interpreted as a record of pedogenesis and geomorphic dynamics, that shaped the soil mantle during the Holocene.

Zhong-Yuan Ren of the Tokyo Institute of Technology and coauthors analyzed trace elements in inclusions of magma solidified within olivine crystals, which recorded the complexities of the magma sources in the mantle during the process of melting, magma uprise, and crystallization.

The authors list several nonbiological processes that could explain their findings, but they favor the idea that the graphite started out as organic matter in sediments that got dragged into the Earth's mantle during the collision of tectonic plates.

The results suggest heterogeneity of H2O content in the upper mantle during the early history of the Earth and raise the question of how much H2O is present in current arc magmas.

We thus assume that dust particles are ejected not only from the active regions but also from the dust mantle by the sublimation of water vapor that passes through the dust mantle during the sublimation process.

Unlike the Dallas Cowboys, who grabbed that mantle during the 1970s with a god-fearing coach and quarterback, barely dressed cheerleaders and a dynamic, winning squad, the Bengals embody what makes the National Football League the most dominant force in our country's sports landscape the impenetrable fortress and a measuring stick by which all other professional leagues are measured.

The considerable height of the Colorado Plateau, for instance, appears to be the result of the warming of the underlying mantle during roughly the past 10 million years.

Half of the Lg wave energy loss occurs as a result of escaping energy into the mantle during propagation in the thinner crustal waveguide (see the gray points in Figure 14 for the dry-sea model), and the other half of the energy attenuation is associated with transfer of Lg wave energy into P waves in seawater (see the red points for the full-sea model).

The whole sequence is completed with transitional swampy deposits, accumulated probably during the MIS3/MIS2 transition, and the typical loess of the Tezanos Pinto Formation, mantled during the Last Maximum Glacial.

This starting model is, of course, a simplification of what is undoubtedly a complex structure of the California margin that has had a long history of accretion of oceanic sediment, mafic crust and ultramafic mantle during subduction in the late Mesozoic and early Tertiary.

Collectively, the Ethiopian data show that the distribution of mantle melts during the initiation of magma assisted rifting is fundamentally influenced by lithospheric structures formed during earlier syn-rift stretching.