Kimberlites are volatile-rich, occasionally diamond-bearing magmas that have erupted
explosively at Earth's surface in the geologic past,–. These enigmatic magmas, originating …

The radiogenic isotope heterogeneity of oceanic basalts is often assessed using 2D isotope
ratio diagrams. But because the underlying data are at least six dimensional (87Sr/86Sr …

Abstract The Pacific Plate is the largest oceanic plate on the Earth since Mesozoic, but its
original mechanism, structure and tectonic evolution are still unclear. The complexity of the …

Volcanism far from plate boundaries is often attributed to an underlying mantle plume,,,,,.
However, enigmatic observations of Hawaiian volcanism, such as variations in the volume of …

Using recently published global magnetic models, we present the first independent
constraint on North Atlantic geothermal state and mantle dynamics from magnetic anomaly …

The large low shear‐wave velocity provinces (LLSVP) are thermochemical anomalies in the
deep Earth's mantle, thousands of km wide and∼ 1800 km high. This study explores the …

Subsidence and uplift patterns and thermal history of sedimentary basins are controlled by
tectonics, mantle dynamics and surface processes, such as erosion, sediment transport and …

The geochemistry of oceanic intraplate (primarily oceanic island and seamount) lavas can
provide essential information on the composition and evolution of their mantle source and …

Abstract In Turonian/Coniacian time a major plate reorganization occurred in Pacific Ocean
that resulted in synchronous climax of compression in Eastern Asia. At this time the …

太**洋板块是一个中生代以来形成的地球上最大的大洋板块, 但其起源机制, 结构构造,
构造演化等始终不清楚. 太**洋板块内部的复杂性更是未受到重视, 其内部的大火成岩省 …