Results 151 to 160 of about 2,903 (264)
Onset of slab mantle melting in Earth's lower mantle: Evidence from ferropericlase in superdeep diamonds. [PDF]
Ni P +15 more
europepmc +1 more source
A shallow mantle source for the Chang'e 5 lavas reveals how top-down heating prolonged lunar magmatism. [PDF]
Elardo SM +4 more
europepmc +1 more source
Geological reactive systems from the mantle to the abyssal sub-seafloor: Preface
Marguerite Godard +3 more
openalex +2 more sources
South Pole-Aitken massive impact 4.25 billion years ago revealed by Chang'e-6 samples. [PDF]
Su B +14 more
europepmc +1 more source
Abstract The Armenian Highlands, a tectonically active segment of the Arabia‐Eurasia collision zone, exhibit widespread Quaternary volcanism, rapid uplift, and intense seismicity. However, the lithospheric processes driving these phenomena remain poorly understood.
Ivan Koulakov +5 more
wiley +1 more source
Ru and W isotope systematics in ocean island basalts reveals core leakage. [PDF]
Messling N +6 more
europepmc +1 more source
Olivine‐Ahrensite Phase Relations in the Mg2SiO4‐Fe2SiO4 System as a Function of Temperature
Abstract Olivine and ahrensite are the primary components of the interiors of Fe‐rich terrestrial planets and meteorites, making their phase relations crucial for planetary science. Moreover, their phase relations can be used for calibrating large‐volume high‐pressure devices such as multi‐anvil apparatus.
Artem Chanyshev +12 more
wiley +1 more source
Reply to: Reassessing gas generation from oil thermal cracking associated with the Emeishan Large Igneous Province. [PDF]
Chen C +6 more
europepmc +1 more source
Abstract The Martian lava plains are characterized by their extensive, low‐relief surfaces, which are the result of numerous basaltic eruptions and feature a variety of volcanic landforms, including vents, cones, pits, and skylights. The combination of these features and impact craters yields a significant understanding of the planet's geological past ...
G. Nodjoumi +4 more
wiley +1 more source

