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Anders Meibom

Researcher at École Polytechnique Fédérale de Lausanne

Publications -  286
Citations -  13247

Anders Meibom is an academic researcher from École Polytechnique Fédérale de Lausanne. The author has contributed to research in topics: Chondrite & Chondrule. The author has an hindex of 56, co-authored 268 publications receiving 11565 citations. Previous affiliations of Anders Meibom include University of Paris & University of Hawaii.

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Growth mechanism and additional constraints on FeNi metal condensation in the solar nebula

TL;DR: In this article, the authors observed a linear correlation between the apparent diameter of the zoned FeNi metal grains and their inferred condensation temperature interval, which indicates that the grain growth rate was essentially constant.
Journal Article

Granitic magmatism on the early Paleozoic UHP belt of northern Qaidam, NW China

TL;DR: Three types of granite association were found on the northern margin of the Qadaim Basin, which is an early Paleozoic ultrahigh pressure metamorphic belt with the eclogite ages of 466-495 Ma as discussed by the authors.
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Short-Term Thermal Acclimation Modifies the Metabolic Condition of the Coral Holobiont

TL;DR: It is suggested that the disconnect that occurred between symbiont bicarbonate and nitrate assimilation in the absence of photosynthetic breakdown in the warm-acclimated corals represents either a shift in nitrogen utilisation, or supply limitation by the host.
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Shock melts in QUE 94411, Hammadah al Hamra 237, and Bencubbin: Remains of the missing matrix?

TL;DR: In this article, the authors studied the petrographical and mineralogical effects of the shock processing that these meteorite assemblages have undergone, and they inferred that hydrated, fine-grained material was originally present between the Fe,Ni-metal grains and chondrules, but was preferentially shock melted.
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Micro‐ to nanostructure and geochemistry of extant crinoidal echinoderm skeletons

TL;DR: Data from micro- to nanostructural and geochemical analyses of calcitic skeletons from extant deep-sea stalked crinoids suggest that physiological factors play an important role in controlling Mg content in crinoid skeletons and that great care should be taken when using their skeletons to reconstruct, for example, palaeotemperatures and Mg/Ca palaeo-variations of the ocean.