Protracted core formation and impact disruptions shaped the earliest outer Solar System planetesimals. [PDF]
Grewal DS +5 more
europepmc +1 more source
Ultra-depleted mantle source of basalts from the South Pole-Aitken basin. [PDF]
Zhou Q +17 more
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Determination of the P-T conditions and depths of magma storage zones for two distinct quaternary lava flows in the Southeast of Mount Ağrı (Eastern Anatolia, Turkey). [PDF]
Dogan-Kulahci GD.
europepmc +1 more source
Recent progress and future prospects of the early solar system chronology. [PDF]
Amelin Y, Yin QZ.
europepmc +1 more source
The Ni isotopic composition of Ryugu reveals a common accretion region for carbonaceous chondrites. [PDF]
Spitzer F +90 more
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Enstatite chondrite and related Earth models
Wade, J, Wood, B, Elliott, T, Walter, M
openaire +1 more source
Silicon Isotope Evidence Against an Enstatite Chondrite Earth
Building Blocks of Earth Earth formed from an explosive and energetic series of collisions that accreted material over millions of years. Comparisons between rocks from Earth's interior and more primitive extraterrestrial samples can help tease apart the composition of Earth's starting material; however, discrepancies between the
Bernard Bourdon, Caroline Fitoussi
exaly +6 more sources
Two meteoritic stones weighing roughly 600 and 200 g fell on 14 April 1942 near Parsa, Bihar, India. The meteorite is a high‐Fe (EH) enstatite chondrite on the basis of its large abundance of chondrules, its low concentrations of refractory elements, the Si content of its metal (25–30 mg/g), and its enstatite composition Mg0.975Ca0.007Fe0.018. The high
N. Bhandari, V. B. Shah, J. T. Wasson
semanticscholar +4 more sources
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Lewis Cliff 87223, an anomalous enstatite chondrite and the diversity of enstatite chondrites
Meteoritics & Planetary Science, 2023We studied a thin section of Lewis Cliff (LEW) 87223, an unusual EL3‐related, enstatite chondrite (EC) that has primary and secondary features not observed in other ECs. We studied its metal‐rich nodules, possible shock features, and chondrules, eight of
K. Goss +3 more
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The Unequilibrated Enstatite Chondrites
Chemie Der Erde, 2012Abstract The enstatite chondrites formed under highly reducing (and/or sulfidizing) conditions as indicated by their mineral assemblages and compositions, which are sharply different from those of other chondrite groups. Enstatite is the major silicate mineral.
Michael K. Weisberg, Makoto Kimura
exaly +2 more sources

