Lithological and isotopic heterogeneity in the mantle archive the mantle's melting history and
fingerprint crustal recycling processes coupling the deep Earth with the terrestrial biosphere …

Lithological heterogeneity is a widely accepted feature of the Earth's mantle, with recycled
crustal material accounting for a significant part of heterogeneity in ocean island basalt (OIB) …

Anhedral metal grains of> micrometer size occur in many lunar rock types, including mare
basalts, magnesian suite rocks (MGS), ferroan anorthosites (FAN), and impact melt rocks …

Constraining the heterogeneity of oxygen fugacity (fO 2) in the upper mantle is important for
understanding the role of the deep Earth in determining the redox state of the atmosphere …

Noble gas isotope systematics of ocean island basalts (OIB) provide evidence for relatively
undegassed and primitive mantle sources. These OIB sources partly derive from the deep …

Fractionation of sulfides during ascent of mantle-derived magmas distributes sulfur and
chalcophile elements into the Earth's lithosphere. It has been suggested that continental …

This study presents Ba isotope compositions of ocean island basalts (OIB) from the Azores
Archipelago to investigate the origin of the enriched components within their mantle sources …

Oxygen fugacity (fO 2) is a fundamental variable in igneous petrology with utility as a
potential tracer of recycled high Fe+ 3/ΣFe surficial materials in the sources of mantle …

The Cenozoic subalkaline to alkaline volcanic rocks from the Eastern Pontides Orogenic
Belt (EPOB) in NE Turkey exhibit wide range of highly siderophile element (HSE) contents …

Continental flood basalts are more prone to compositional modification from passage
through thicker and (or) more felsic crust in comparison to their oceanic counterparts. The …