| Microplastics contaminate the deepest part of the world's ocean |
42 |
| W-182 evidence or core-mantle interaction in the source of mantle plumes |
19 |
| Mass-dependent triple oxygen isotope variations in terrestrial materials |
16 |
| A stochastic sampling approach to zircon eruption age interpretation |
14 |
| Oxygen minimum zones in the early Cambrian ocean |
13 |
| Silicon and oxygen isotopes unravel quartz formation processes in the Icelandic crust |
11 |
| Onset of new, progressive crustal growth in the central Slave craton at 3.55 Ga |
11 |
| Large oxygen excess in the primitive mantle could be the source of the Great Oxygenation Event |
10 |
| Chemical nature of the 3.4 Ga Strelley Pool microfossils |
9 |
| Bridging the depleted MORB mantle and the continental crust using titanium isotopes |
9 |
| Mobility of chromium in high temperature crustal and upper mantle fluids |
9 |
| Oxidised micrometeorites as evidence for low atmospheric pressure on the early Earth |
8 |
| Magma properties at deep Earth's conditions from electronic structure of silica |
8 |
| Noble gases and nitrogen in Tissint reveal he composition of the Mars atmosphere |
7 |
| Goethite, a tailor-made host for the critical metal scandium: The FexSc(1-x)OOH solid solution |
7 |
| Onset of volatile recycling into the mantle determined by xenon anomalies |
7 |
| Calcium stable isotopes place Devonian conodonts as first level consumers |
6 |
| Hadean geodynamics inferred from time-varying Nd-142/Nd-144 in the early Earth rock record |
6 |
| Experimental evidence for fluid-induced melting in subduction zones |
5 |
| Properties of molten CaCO3 at high pressure |
5 |
| Exchange catalysis during anaerobic methanotrophy revealed by (CH2D2)-C-12 by and (CH3D)-C-13 in methane |
5 |
| Hadean protocrust reworking at the origin of the Archean Napier Complex (Antarctica) |
5 |
| An oxygen isotope test for the origin of Archean mantle roots |
4 |
| The xenon isotopic signature of the mantle beneath Massif Central |
4 |
| Mercury reallocation in thawing subarctic peatlands |
4 |
| Experimental clues for detecting biosignatures on Mars |
4 |
| The effect of core segregation on the Cu and Zn isotope composition of the silicate Moon |
4 |
| Apollo 15 green glass He-Ne-Ar signatures - In search for indigenous lunar noble gases |
4 |
| Fluid discharge linked to bending of the incoming plate at the Mariana subduction zone |
4 |
| Toxic anthropogenic pollutants reach the deepest ocean on Earth |
4 |
| Redox state of the convective mantle from CO2-trace element systematics of oceanic basalts |
4 |
| Formation of Archean continental crust constrained by boron isotopes |
4 |
| Abiogenesis not required to explain the origin of volcanic-hydrothermal hydrocarbons |
4 |
| Thermodynamic controls on redox-driven kinetic stable isotope fractionation |
3 |
| Graphite floatation on a magma ocean and the fate of carbon during core formation |
3 |
| Transition metal availability to speleothems controlled by organic binding ligands |
3 |
| Decoupling of dissolved and bedrock neodymium isotopes during sedimentary cycling |
3 |
| The primordial He budget of the Earth set by percolative core formation in planetesimals |
3 |
| Radiogenic Ca isotopes confirm post-formation K depletion of lower crust |
3 |
| A lunar hygrometer based on plagioclase-melt partitioning of water |
3 |
| Sea level rise produces abundant organobromines in salt-affected coastal wetlands |
3 |
| Th/U and U series systematics of saprolite: importance for the oceanic U-234 excess |
3 |
| Atmospheric helium isotopic ratio from 1910 to 2016 recorded in stainless steel containers |
2 |
| Diffusive fractionation of Li isotopes in wet, highly silicic melts |
2 |
| Colloidal origin of microbands in banded iron formations |
2 |
| Ultrahigh pressure structural changes in a 60 mol. % Al2O3-40 mol. % SiO2 glass |
2 |
| Carbon isotopic signatures of super-deep diamonds mediated by iron redox chemistry |
2 |
| Zircon halogen geochemistry: Insights into Hadean-Archean fluids |
2 |
| Pt-190-Os-186 geochronometer reveals open system behaviour of Pt-190-He-4 isotope system |
2 |
| Loss of immiscible nitrogen from metallic melt explains Earth's missing nitrogen |
2 |
