Widespread production of silica- and alkali -rich melts at the onset of planetesimal melting

被引：0
|
作者：
Collinet, Max [1 ]
Grove, Timothy L. [1 ]
机构：
[1] MIT, Earth Atmospher & Planetary Sci Dept, 77 Massachusetts Ave, Cambridge, MA 02139 USA
来源：
GEOCHIMICA ET COSMOCHIMICA ACTA | 2020年 / 277卷
关键词：
GRAVES NUNATAKS 06128; IIE IRON-METEORITES; PARENT BODY; EXPERIMENTAL CONSTRAINTS; PYROCLASTIC VOLCANISM; ORDINARY CHONDRITES; THERMAL EVOLUTION; OXYGEN-ISOTOPE; CORE FORMATION; MAGMA OCEAN;
D O I：
暂无
中图分类号：
P3 [地球物理学]; P59 [地球化学];
学科分类号：
0708 ; 070902 ;
摘要：
引用
收藏
页码：334 / 357
页数：24
相关论文
共 7 条
  • [1] Effect of oxygen fugacity on the glass transition, viscosity and structure of silica- and iron-rich magmatic melts
    Di Genova, Danilo
    Vasseur, Jeremie
    Hess, Kai-Uwe
    Neuville, Daniel R.
    Dingwell, Donald B.
    [J]. JOURNAL OF NON-CRYSTALLINE SOLIDS, 2017, 470 : 78 - 85
  • [2] Melting experiments of an L6 ordinary chondrite: Insights into early planetesimal differentiation and alkali-rich achondrite formation.
    Lelarge, Iannini S.
    Masotta, M.
    Folco, L.
    Ubide, T.
    Suttle, M. D.
    Pittarello, L.
    [J]. METEORITICS & PLANETARY SCIENCE, 2023, 58 : A129 - A129
  • [3] Experimental study of partial melting of mantle peridotite - A discussion about the genesis of silica-rich fluids (melts)
    Li, JP
    Jacques, K
    [J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION, 1999, 73 (04) : 395 - 403
  • [4] Melting and Phase Relations of Carbonated Eclogite at 9-21 GPa and the Petrogenesis of Alkali-Rich Melts in the Deep Mantle
    Kiseeva, Ekaterina S.
    Litasov, Konstantin D.
    Yaxley, Gregory M.
    Ohtani, Eiji
    Kamenetsky, Vadim S.
    [J]. JOURNAL OF PETROLOGY, 2013, 54 (08) : 1555 - 1583
  • [5] Phase relations and melting of carbonated peridotite between 10 and 20 GPa: a proxy for alkali- and CO2-rich silicate melts in the deep mantle
    Ghosh, Sujoy
    Litasov, Konstantin
    Ohtani, Eiji
    [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 2014, 167 (02) : 1 - 23
  • [6] Phase relations and melting of carbonated peridotite between 10 and 20 GPa: a proxy for alkali- and CO2-rich silicate melts in the deep mantle
    Sujoy Ghosh
    Konstantin Litasov
    Eiji Ohtani
    [J]. Contributions to Mineralogy and Petrology, 2014, 167
  • [7] Immiscible transition from carbonate-rich to silicate-rich melts in the 3 GPa melting interval of eclogite plus CO2 and genesis of silica-undersaturated ocean island lavas
    Dasgupta, R
    Hirschmann, MM
    Stalker, K
    [J]. JOURNAL OF PETROLOGY, 2006, 47 (04) : 647 - 671
1