Jürgen Eisele

Composition of the depleted mantle

Formation of the 1300-km-wide intracontinental orogen and postorogenic magmatic province in Mesozoic South China: A flat-slab subduction model

East Molokai and other Kea‐trend volcanoes: Magmatic processes and sources as they migrate away from the Hawaiian hot spot

Recognizing Mantle Plumes in the Geological Record

Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust

Isotope and trace element variations in lavas from Raivavae and Rapa, Cook–Austral islands: constraints on the nature of HIMU- and EM-mantle and the origin of mid-plate volcanism in French Polynesia

The Lu–Hf and Sm–Nd isotopic composition of CHUR: Constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets

Involvement of Continental Crust in the Formation of the Cretaceous Kerguelen Plateau: New Perspectives from ODP Leg 120 Sites

Recycled metasomatized lithosphere as the origin of the Enriched Mantle II (EM2) end‐member: Evidence from the Samoan Volcanic Chain

Geochemical segmentation of the Mid‐Atlantic Ridge north of Iceland and ridge–hot spot interaction in the North Atlantic

Recycling oceanic crust: Quantitative constraints

Major and trace element composition of the depleted MORB mantle (DMM)

The 320 kyr Pb isotope evolution of Mauna Kea lavas recorded in the HSDP‐2 drill core

The role of sediment recycling in EM-1 inferred from Os, Pb, Hf, Nd, Sr isotope and trace element systematics of the Pitcairn hotspot