Pages that link to "Q28262020"

The following pages link to Late formation and prolonged differentiation of the Moon inferred from W isotopes in lunar metals (Q28262020):

Displayed 50 items.

• Targeting DNA topoisomerase II in cancer chemotherapy (Q24649711) ‎ (← links)
• Structural insight into the quinolone-DNA cleavage complex of type IIA topoisomerases (Q27655501) ‎ (← links)
• Structural basis of quinolone inhibition of type IIA topoisomerases and target-mediated resistance (Q27664216) ‎ (← links)
• Timing of crystallization of the lunar magma ocean constrained by the oldest zircon (Q28314942) ‎ (← links)
• The Astrobiology Primer v2.0 (Q28596454) ‎ (← links)
• The iodine-plutonium-xenon age of the Moon-Earth system revisited (Q28654682) ‎ (← links)
• Isotopes as clues to the origin and earliest differentiation history of the Earth (Q33372996) ‎ (← links)
• Laboratory technology and cosmochemistry (Q33875154) ‎ (← links)
• A planetary perspective on the deep Earth (Q34009463) ‎ (← links)
• Lunar-forming impacts: processes and alternatives (Q34025946) ‎ (← links)
• Geochemical arguments for an Earth-like Moon-forming impactor (Q34025959) ‎ (← links)
• Rb-Sr, Sm-Nd and Lu-Hf isotope systematics of the lunar Mg-suite: the age of the lunar crust and its relation to the time of Moon formation (Q34025963) ‎ (← links)
• Siderophile element constraints on the origin of the Moon (Q34025991) ‎ (← links)
• Evaporative fractionation of volatile stable isotopes and their bearing on the origin of the Moon (Q34025998) ‎ (← links)
• Lunar exploration: opening a window into the history and evolution of the inner Solar System (Q34026004) ‎ (← links)
• Zinc isotopic evidence for the origin of the Moon (Q34306730) ‎ (← links)
• Forming a Moon with an Earth-like composition via a giant impact. (Q34306741) ‎ (← links)
• Identification of the giant impactor Theia in lunar rocks (Q34423271) ‎ (← links)
• Lunar formation. Dating the Moon-forming impact event with asteroidal meteorites (Q34472214) ‎ (← links)
• A young Moon-forming giant impact at 70-110 million years accompanied by late-stage mixing, core formation and degassing of the Earth (Q34841245) ‎ (← links)
• Heterogeneity in lunar anorthosite meteorites: implications for the lunar magma ocean model (Q35223234) ‎ (← links)
• Fast accretion of the earth with a late moon-forming giant impact (Q35470844) ‎ (← links)
• Terrestrial planet formation (Q35585886) ‎ (← links)
• The chlorine isotope fingerprint of the lunar magma ocean (Q35851165) ‎ (← links)
• Quantitative interactome analysis reveals a chemoresistant edgotype (Q35941833) ‎ (← links)
• Growing the terrestrial planets from the gradual accumulation of submeter-sized objects (Q36306019) ‎ (← links)
• Early formation of the Moon 4.51 billion years ago. (Q37580468) ‎ (← links)
• Isotopes as tracers of the sources of the lunar material and processes of lunar origin. (Q38239097) ‎ (← links)
• The giant impact hypothesis: past, present (and future?). (Q38239099) ‎ (← links)
• A primordial origin for the compositional similarity between the Earth and the Moon (Q38427156) ‎ (← links)
• Tungsten isotopic evidence for disproportional late accretion to the Earth and Moon (Q38427164) ‎ (← links)
• Lunar tungsten isotopic evidence for the late veneer (Q38427172) ‎ (← links)
• D/H ratios of the inner Solar System. (Q38431847) ‎ (← links)
• Lunar and terrestrial planet formation in the Grand Tack scenario (Q38435335) ‎ (← links)
• New approaches to the Moon's isotopic crisis (Q38435354) ‎ (← links)
• Highly siderophile elements in Earth's mantle as a clock for the Moon-forming impact (Q38439702) ‎ (← links)
• Planetary science: Lunar conspiracies (Q38443871) ‎ (← links)
• Hydrogen isotopes in lunar volcanic glasses and melt inclusions reveal a carbonaceous chondrite heritage (Q38450544) ‎ (← links)
• Planetary science. The origin of the Moon (Q38456165) ‎ (← links)
• Making the Moon from a fast-spinning Earth: a giant impact followed by resonant despinning (Q38457298) ‎ (← links)
• Hf-W-Th evidence for rapid growth of Mars and its status as a planetary embryo (Q38463495) ‎ (← links)
• Silicon isotope evidence against an enstatite chondrite Earth (Q38464838) ‎ (← links)
• Stochastic late accretion to Earth, the Moon, and Mars (Q38465540) ‎ (← links)
• Heterogeneous accretion and the moderately volatile element budget of Earth. (Q38468137) ‎ (← links)
• Volatile accretion history of the terrestrial planets and dynamic implications (Q38470663) ‎ (← links)
• Chronological evidence that the Moon is either young or did not have a global magma ocean (Q38471275) ‎ (← links)
• Early differentiation of the Earth and the Moon. (Q38475615) ‎ (← links)
• Volatile accretion history of the Earth. (Q38480253) ‎ (← links)
• The lead isotopic age of the Earth can be explained by core formation alone (Q38484676) ‎ (← links)
• The Earth's missing lead may not be in the core (Q38498060) ‎ (← links)