地球科学と気候変動ジャーナル

抽象的な

Introduction for the article assortment "High-Pressure Earth and Planetary Science in the last and one decade from now"

Yamini Sai

Goliath sway occasions during planetary growth caused huge levels of liquefying of the early Earth. the volumes of soften, pressing factor, and temperature states of metal-silicate equilibration after each effect, and showed that the pressing factor development during metal-silicate equilibration during accumulation relies emphatically upon the lifetime of effect created magma seas contrasted with the time span between huge effects structure of an early Earth repository (EER) with the guide of 142Nd/144Nd isotope systematics to decide the age and pressing factor temperature conditions to frame the EER