The participation of ilmenite-bearing cumulates in lunar mantle overturn

Autor: Michael H. G. Jacobs, A. P. van den Berg, J. de Vries, W. van Westrenen, Y. Zhao

Publikováno v: Zhao, Y, De Vries, J, van den Berg, A P, Jacobs, M H G & van Westrenen, W 2019, ' The participation of ilmenite-bearing cumulates in lunar mantle overturn ', Earth and Planetary Science Letters, vol. 511, pp. 1-11 . https://doi.org/10.1016/j.epsl.2019.01.022
Earth and Planetary Science Letters, 511, 1-11. Elsevier
Earth and Planetary Science Letters, 511, 1. Elsevier

The ilmenite-bearing cumulates (IBC) formed from the solidification of the lunar magma ocean are thought to have significantly affected the long-term evolution of the lunar interior and surface. Their high density is considered to trigger Rayleigh–

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ea8443ce728a8d339409634ef5c42131
https://research.vu.nl/en/publications/1df382eb-a41e-4239-9cfd-ebe64c1d99ac

Small-scale mineralogical heterogeneity from variations in phase assemblages in the transition zone and D″ layer predicted by convection modelling

Autor: Michael H. G. Jacobs, Maarten V. de Hoop, David A. Yuen, Arie P. van den Berg

Publikováno v: Journal of Earth Science. 22:160-168

Small-scale heterogeneity in the deep mantle is concentrated in the upper-mantle transition zone (TZ), in the depth range 410–660 km and also at the bottom 250 km D″ region. This encourages a more detailed investigation of the potential for seism

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::a4b7114aadd7ef9e2400b0a423087d12
https://doi.org/10.1007/s12583-011-0168-7

Thermodynamics and diffusion in ternary Fe–Al–Cr alloys, Part I: Thermodynamic modeling

Autor: Rainer Schmid-Fetzer, Günter Borchardt, Karl-Heinz Spitzer, Michael H. G. Jacobs, V. B. Motalov, Torsten Markus

Publikováno v: Intermetallics. 16:995-1005

The development of an accurate thermodynamic model description for the system Fe–Al–Cr is hampered by the sparseness of thermodynamic data in this ternary system. This compelled us to measure activities in the system Fe–Al–Cr using the Knudse

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::765361e3a4ed080b8ac7841c7989a2c2
https://doi.org/10.1016/j.intermet.2008.04.020

Host Atom Diffusion in Ternary Fe-Cr-Al Alloys

Autor: Lars Dörrer, Rainer Schmid-Fetzer, Anna J. Kulińska, Diana Rohrberg, Michael H. G. Jacobs, Karl-Heinz Spitzer, Günter Borchardt, Anna Fraczkiewicz, Torsten Markus

Publikováno v: Metallurgical and Materials Transactions A
Metallurgical and Materials Transactions A, Springer Verlag/ASM International, 2014, 45A (1), pp.269-279. ⟨10.1007/s11661-013-1967-5⟩

International audience; In the Fe-rich corner of the Fe-Cr-Al ternary phase diagram, both interdiffusion experiments [1048 K to 1573 K (775 degrees C to 1300 degrees C)] and Fe-58 tracer diffusion experiments [873 K to 1123 K (600 degrees C to 850 de

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c8b833fc8e6785cfb476c3b7f894d778
https://hal-emse.ccsd.cnrs.fr/emse-01066893

Thermal equation of state of synthetic orthoferrosilite at lunar pressures and temperatures

Autor: J. de Vries, Michael H. G. Jacobs, M. Wehber, Catherine McCammon, A. P. van den Berg, W. van Westrenen, Christian Lathe

Publikováno v: Physics and Chemistry of Minerals
de Vries, J, Jacobs, J M G, van den Berg, A P, Wehber, M, Lathe, C, McCammon, C A & van Westrenen, W 2013, ' Thermal equation of state of synthetic orthoferrosilite at lunar pressures and temperatures ', Physics and Chemistry of Minerals, no. 40, pp. 691-703 . https://doi.org/10.1007/s00269-013-0605-5
Physics and Chemistry of Minerals, 691-703. Springer Verlag
ISSUE=40;STARTPAGE=691;ENDPAGE=703;ISSN=0342-1791;TITLE=Physics and Chemistry of Minerals
Physics and Chemistry of Minerals, 40(9), 691. Spinger

Iron-rich orthopyroxene plays an important role in models of the thermal and magmatic evolution of the Moon, but its density at high pressure and high temperature is not well-constrained. We present in situ measurements of the unit-cell volume of a s

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::308aeae7ab8725d325257fb5ac26afd7
http://doi.crossref.org/servlet/query?format=unixref&pid=bib@gfz-potsdam.de&id=10.1007/s00269-013-0605-5