Results 201 to 210 of about 65,526 (293)

Upper mantle low-velocity layer tied to volatile-charged carbonate melts. [PDF]

open access: yesSci Adv
Huang Y   +6 more
europepmc   +1 more source

A Common Reference Material for Mass‐Dependent Sn Isotope Compositions: An Inter‐Laboratory Calibration Approach

open access: yesGeostandards and Geoanalytical Research, Volume 50, Issue 2, Page 341-367, June 2026.
Key Points We recommend using the notation δ122/118SnNIST SRM 3161a for mass‐dependent Sn isotope data. We derived conversion factors relative to NIST SRM 3161a for Puri Sn CEZA (0.132 ± 0.011‰), Sn Lyon (0.229 ± 0.016‰), Sn IPGP (0.162 ± 0.018‰). Tin isotope compositions are presented for SPEX CertiPrep Sn and nine USGS reference materials.
Aurélia C.E. Meister   +10 more
wiley   +1 more source

Kinding Culture

open access: yesJournal for the Theory of Social Behaviour, Volume 56, Issue 2, June 2026.
ABSTRACT Progress and dialogue in cultural analysis are often hindered by analysts' reliance on implicit ontic claims, namely, foundational, unstated assumptions about the expected properties and typical characteristics of cultural kinds, thus precluding proper debate and theoretical progress.
Omar Lizardo
wiley   +1 more source

Lens effect of remnant blocks on deep mantle upwelling causing anomalous subsidence. [PDF]

open access: yesNat Commun
Liu L   +7 more
europepmc   +1 more source

Combustion and Pyrolysis EA‐IRMS Techniques to Determine the δ2H of Diamonds

open access: yesRapid Communications in Mass Spectrometry, Volume 40, Issue 10, 30 May 2026.
ABSTRACT Rationale Diamonds are generally considered to be metasomatic minerals originating from the Earth's mantle. They formed through the interaction of carbon‐bearing fluids or melts with the surrounding deep lithology. Most knowledge about the formation of diamonds comes from studying their mineral inclusions or stable isotopes.
François Fourel   +4 more
wiley   +1 more source

Ultra-depleted mantle source of basalts from the South Pole-Aitken basin. [PDF]

open access: yesNature
Zhou Q   +17 more
europepmc   +1 more source

The Fate of Iron Formations in the Deep Mantle: Constraints From Iron Oxide Reduction Kinetics Experiments

open access: yesGeophysical Research Letters, Volume 53, Issue 10, 28 May 2026.
Abstract Dense sedimentary iron formations (IFs) subducted into the mantle during Earth's early history, may have descended to the core‐mantle boundary where they could exert strong control on its thermal and seismological properties. A key unanswered question is the extent to which IFs retain their oxidized character in the much more reducing mantle ...
Jemila A. Edmond   +2 more
wiley   +1 more source

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