Geophysically detectible mid-lithospheric discontinuities (MLD) and lithosphere-
asthenosphere boundaries (LAB) beneath cratons have received much attention over recent …

Earth as an Evolving Planetary System, Fourth Edition discusses key topics dealing with the
evolution and interaction through time of Earth's crust, mantle, core, atmosphere …

New versions of the universal Jd-Di exchange clinopyroxene barometer for peridotites,
pyroxenites and eclogites, and also garnet barometer for eclogites and peridotites were …

The 650–621 Ma plume which impinged beneath the Siberian craton during the breakup of
Rodinia caused the formation of several alkaline carbonatite massifs in craton margins of the …

Abstract We report Re–Os and platinum group element (PGE) systematics for a suite of 16
mantle peridotites from the Udachnaya (360 Ma) and Obnazhennaya (160 Ma) kimberlite …

Mineral data from Yakutian kimberlites allow reconstruction of the history of lithospheric
mantle. Differences occur in compositions of mantle pyropes and clinopyroxenes from large …

Cratons represent modern Earth's thickest, coldest, and most depleted lithospheres.
Reintroduction of volatiles led to gradual reoxidation and refertilization of initially highly …

The pressure-temperature (PT) conditions and position of different groups of eclogites in the
sub-cratonic lithospheric mantle (SCLM) worldwide were established using clinopyroxene …

Microinclusions of high-density fluids (HDF's) occur in cloudy diamonds from the Mir and
Internatsionalnaya kimberlite pipes (Malobotuobia kimberlite field, Siberian platform). These …

We have studied variations in the structure and composition of minerals from the pipes of the
Yakutian kimberlite province (YKP) in different mantle terranes of the Siberian craton. The …