Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Max Collinet"'
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 11, Pp n/a-n/a (2023)
Abstract The composition of basaltic melts in equilibrium with the mantle can be determined for several Martian meteorites and in‐situ rover analyses. We use the melting model MAGMARS to reproduce these primary melts and estimate the bulk compositi
Externí odkaz:
https://doaj.org/article/d6c497ebc7884773b52365ad6bfe3fa1
Autor:
Quancheng Huang, Nicholas C. Schmerr, Scott D. King, Doyeon Kim, Attilio Rivoldini, Ana-Catalina Plesa, Henri Samuel, Ross R. Maguire, Foivos Karakostas, Vedran Lekić, Constantinos Charalambous, Max Collinet, Robert Myhill, Daniele Antonangeli, Mélanie Drilleau, Misha Bystricky, Caroline Bollinger, Chloé Michaut, Tamara Gudkova, Jessica C. E. Irving, Anna Horleston, Benjamin Fernando, Kuangdai Leng, Tarje Nissen-Meyer, Frederic Bejina, Ebru Bozdağ, Caroline Beghein, Lauren Waszek, Nicki C. Siersch, John-Robert Scholz, Paul M. Davis, Philippe Lognonné, Baptiste Pinot, Rudolf Widmer-Schnidrig, Mark P. Panning, Suzanne E. Smrekar, Tilman Spohn, William T. Pike, Domenico Giardini, W. Bruce Banerdt
Publikováno v:
Proceedings of the National Academy of Sciences of the United States of America
Proceedings of the National Academy of Sciences of the United States of America, 2022, 119 (42), ⟨10.1073/pnas.2204474119⟩
Proceedings of the National Academy of Science
Proceedings of the National Academy of Sciences of the United States of America, 119 (42)
Huang, Q, Schmerr, N, Horleston, A C, Irving, J C E, Myhill, R C, Giardini, D & et, A 2022, ' Seismic detection of a deep mantle discontinuity within Mars by InSight ', Proceedings of the National Academy of Sciences of the United States of America, vol. 119, no. 42, e2204474119 . https://doi.org/10.1073/pnas.2204474119
Proceedings of the National Academy of Sciences of the United States of America, 2022, 119 (42), ⟨10.1073/pnas.2204474119⟩
Proceedings of the National Academy of Science
Proceedings of the National Academy of Sciences of the United States of America, 119 (42)
Huang, Q, Schmerr, N, Horleston, A C, Irving, J C E, Myhill, R C, Giardini, D & et, A 2022, ' Seismic detection of a deep mantle discontinuity within Mars by InSight ', Proceedings of the National Academy of Sciences of the United States of America, vol. 119, no. 42, e2204474119 . https://doi.org/10.1073/pnas.2204474119
Constraining the thermal and compositional state of the mantle is crucial for deciphering the formation and evolution of Mars. Mineral physics predicts that Mars' deep mantle is demarcated by a seismic discontinuity arising from the pressure-induced
Autor:
Cyrena A. Goodrich, Max Collinet, Allan Treiman, Tabb C. Prissel, Markus Patzek, Samuel Ebert, Michael J. Jercinovic, Addi Bischoff, Andreas Pack, Jean‐Alix Barrat, Stephan Decker
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e30f9ef4360b715ee12b49c4eb437dad
https://doi.org/10.1111/maps.13889
https://doi.org/10.1111/maps.13889
Autor:
Timothy L. Grove, Max Collinet
Publikováno v:
Geochimica et Cosmochimica Acta. 277:334-357
We present the results of melting experiments on a suite of carbonaceous and ordinary chondritic compositions (CV, CM, CI, H and LL) performed at low pressure (0.1–13.1 MPa) and over a range of oxygen fugacity (log fO2 − (log fO2)IW = −2.5 to
Autor:
Timothy L. Grove, Max Collinet
Publikováno v:
Prof. Grove
© The Meteoritical Society, 2020. Ureilites are carbon-rich ultramafic achondrites that have been heated above the silicate solidus, do not contain plagioclase, and represent the melting residues of an unknown planetesimal (i.e., the ureilite parent
Introduction During the early stages of lunar evolution, the large amount of heat available from the lunar forming impact led to extensive melting of the Moon’s silicate mantle giving rise to a magma ocean. The fractional crystallization of the lat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c421ee03517c1a617f1c036cfe4fa6d8
https://doi.org/10.5194/epsc2021-834
https://doi.org/10.5194/epsc2021-834
Basaltic melts are produced when convection adiabatically brings deep and hot mantle to lower pressures. Such primary melts were extracted from the mantle of Mars, crystallized near the surface and...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f867cc8048efa2528712fc4452c3f222
https://doi.org/10.1002/essoar.10504950.1
https://doi.org/10.1002/essoar.10504950.1