| Mineralogy, early marine diagenesis, and the chemistry of shallow-water carbonate sediments |
38 |
| Strange messenger: A new history of hydrogen on Earth, as told by Xenon |
36 |
| Quantifying early marine diagenesis in shallow-water carbonate sediments |
35 |
| Sector-zoned clinopyroxene as a recorder of magma history, eruption triggers, and ascent rates |
28 |
| Evolution of atmospheric xenon and other noble gases inferred from Archean to Paleoproterozoic rocks |
23 |
| Diagenetic effects on uranium isotope fractionation in carbonate sediments from the Bahamas |
23 |
| Evaporation of moderately volatile elements from silicate melts: experiments and theory |
23 |
| Post-collisional alkaline magmatism as gateway for metal and sulfur enrichment of the continental lower crust |
21 |
| Modeling uranium(VI) adsorption onto montmorillonite under varying carbonate concentrations: A surface complexation model accounting for the spillover effect on surface potential |
21 |
| Secular mantle oxidation across the Archean-Proterozoic boundary: Evidence from V partitioning in komatiites and picrites |
20 |
| Geochemical and micro-textural fingerprints of boiling in pyrite |
20 |
| The chemical composition of carbonaceous chondrites: Implications for volatile element depletion, complementarity and alteration |
20 |
| Sulfate-reducing bacteria influence the nucleation and growth of mackinawite and greigite |
20 |
| Hf-W chronology of CR chondrites: Implications for the timescales of chondrule formation and the distribution of Al-26 in the solar nebula |
19 |
| Formation of hydrothermal tin deposits: Raman spectroscopic evidence for an important role of aqueous Sn(IV) species |
19 |
| Time and duration of chondrule formation: Constraints from Al-26-(26) Mg ages of individual chondrules |
19 |
| The effects of diagenesis on geochemical paleoredox proxies in sedimentary carbonates |
19 |
| Elemental and isotopic variability in solar system materials by mixing and processing of primordial disk reservoirs |
18 |
| Microbially mediated nitrate-reducing Fe(II) oxidation: Quantification of chemodenitrification and biological reactions |
18 |
| Controls of eustasy and diagenesis on the U-238/U-235 of carbonates and evolution of the seawater (U-234/U-238) during the last 1.4 Myr |
17 |
| Molybdenum isotope fractionation during adsorption to organic matter |
17 |
| Origin of depleted basalts during subduction initiation and early development of the Izu-Bonin-Mariana island arc: Evidence from IODP expedition 351 site U Amami-Sankaku basin |
16 |
| A model for the oceanic mass balance of rhenium and implications for the extent of Proterozoic ocean anoxia |
16 |
| Coupled Mo-U abundances and isotopes in a small marine euxinic basin: Constraints on processes in euxinic basins |
16 |
| Modern rather than Mesoarchaean oxidative weathering responsible for the heavy stable Cr isotopic signatures of the 2.95 Ga old Ijzermijn iron formation (South Africa) |
15 |
| Mechanisms of electron transfer from structrual Fe(II) in reduced nontronite to oxygen for production of hydroxyl radicals |
15 |
| Modelling the mercury stable isotope distribution of Earth surface reservoirs: Implications for global Hg cycling |
15 |
| Annealing kinetics of radiation damage in zircon |
15 |
| Carbonic anhydrase, coral calcification and a new model of stable isotope vital effects |
15 |
| Revisiting the effects of hydrodynamic sorting and sedimentary recycling on chemical weathering indices |
15 |
| Dynamics of pyrite formation and organic matter sulfurization in organic-rich carbonate sediments |
14 |
| High abundances of presolar grains and N-15-rich organic matter in CO3.0 chondrite Dominion Range 08006 |
14 |
| The role of iron and reactive oxygen species in the production of CO2 in arctic soil waters |
14 |
| Thallium (Tl) sorption onto illite and smectite: Implications for Tl mobility in the environment |
14 |
| Experimental constraints on Li isotope fractionation during clay formation |
14 |
| Calcium isotope fractionation during magmatic processes in the upper mantle |
14 |
| Extended Deep Earth Water Model for predicting major element mantle metasomatism |
14 |
| W-182 and HSE constraints from 2.7 Ga komatiites on the heterogeneous nature of the Archean mantle |
14 |
| Multiple sulfur isotopes monitor fluid evolution of an Archean orogenic gold deposit |
14 |
| Barium isotopic composition of the upper continental crust |
14 |
| Pore-scale numerical investigation of the impacts of surface roughness: Upscaling of reaction rates in rough fractures |
14 |
| Mercury transformations in resuspended contaminated sediment controlled by redox conditions, chemical speciation and sources of organic matter |
14 |
| Dual isotope evidence for sedimentary integration of plant wax biomarkers across an Andes-Amazon elevation transect |
13 |
| Halogens, trace element concentrations, and Sr-Nd isotopes in apatite from iron oxide-apatite (IOA) deposits in the Chilean iron belt: Evidence for magmatic and hydrothermal stages of mineralization |
13 |
| Updated calibration of the clumped isotope thermometer in planktonic and benthic foraminifera |
13 |
| Formation of CV chondrules by recycling of amoeboid olivine aggregate-like precursors |
13 |
| Formation of abiotic hydrocarbon from reduction of carbonate in subduction zones: Constraints from petrological observation and experimental simulation |
13 |
| Calcium isotope evidence for subduction-enriched lithospheric mantle under the northern North China Craton |
13 |
| Ferrihydrite interaction with silicate and competing oxyanions: Geometry and Hydrogen bonding of surface species |
13 |
| Evaluating the fidelity of the cerium paleoredox tracer during variable carbonate diagenesis on the Great Bahamas Bank |
13 |
