Pages that link to "Q38427172"
Jump to navigation
Jump to search
The following pages link to Lunar tungsten isotopic evidence for the late veneer (Q38427172):
Displayed 16 items.
- Oxygen isotopic evidence for vigorous mixing during the Moon-forming giant impact. (Q34511317) (← links)
- Tungsten isotopic constraints on the age and origin of chondrules. (Q36710656) (← links)
- An asteroidal origin for water in the Moon (Q36974086) (← links)
- The isotopic nature of the Earth's accreting material through time (Q38406355) (← links)
- Age of Jupiter inferred from the distinct genetics and formation times of meteorites (Q38430588) (← links)
- The lunar core can be a major reservoir for volatile elements S, Se, Te and Sb. (Q46122872) (← links)
- Early episodes of high-pressure core formation preserved in plume mantle. (Q49716905) (← links)
- An incredible likeness of being (Q58927183) (← links)
- A multiple-impact origin for the Moon (Q59477149) (← links)
- Siderophile element constraints on the thermal history of the H chondrite parent body (Q63495022) (← links)
- Heterogeneous delivery of silicate and metal to the Earth by large planetesimals (Q63495029) (← links)
- Tungsten Isotopes in Planets (Q63495058) (← links)
- Siderophile Elements in Tracing Planetary Formation and Evolution (Q63495071) (← links)
- Effects of core formation on the Hf-W isotopic composition of the Earth and dating of the Moon-forming impact (Q92860942) (← links)
- A long-lived magma ocean on a young Moon (Q97646417) (← links)
- Analytical Model for the Tidal Evolution of the Evection Resonance and the Timing of Resonance Escape (Q100519249) (← links)