Trace Element Geochemistry of a Lunar Granulite: Evidence from Northwest Africa 3163

Trace element geochemistry of the 1991 Mt. Pinatubo silicic melts, Philippines: Implications for ore-forming potential of adakitic magmatism

Trace element geochemistry of the Louis Lake batholith of early Precambrian age, Wyoming

Trace element geochemistry of the peridotite-gabbro-basalt suite from DSDP Leg 37

Trace element identification of three chemically distinct very low titanium (VLT) basalt glasses from Apollo 17

Trace element partition coefficients for clinopyroxene and phlogopite in an alkaline lamprophyre from Newfoundland by LAM-ICP-MS

Trace element partition patterns in North Atlantic deep-sea sediments

Trace element partitioning and melt structure: An experimental study at 1 atm pressure

Trace Element Partitioning Between Low-Calcium Pyroxene and Lunar Picritic Glass Melts at Multiple-Saturation Points with Applications to Melting and Melt Migration in A Heterogeneous Lunar Cumulate Mantle

Trace element partitioning between taenite and kamacite - Relationship to the cooling rates of iron meteorites

Trace element partitioning between type B CAI melts and melilite and spinel: Implications for trace element distribution during CAI formation

Trace Element Partitioning in Porphyritic, Pyroxene-rich Chondrules in Semarkona

Trace Element Partitioning in the Fe-Ni-P System: Applications to P-rich Iron Meteorites

Trace element partitioning in the Fe-S-C system and its implications for planetary differentiation and the thermal history of ureilites

Trace element signature of subduction-zone fluids, melts and supercritical liquids at 120-180km depth

Trace Element Signatures in the Apollo 14 High-Al Basalts: What Do They Represent?

Trace element study of high- and low-refractive index Muong Nong-type tektites from Indochina

Trace element transport during dehydration processes in the subducted oceanic crust: 1. Experiments and implications for the origin of ocean island basalts

Trace element transport rates in subduction zones: evidence from Th, Sr and Pb isotope data for Tonga-Kermadec arc lavas

Trace Element Variability of the Apollo 14 High-Al Basalts: A Result of Igneous Processes or Sample Size?