Petrography,mineral chemistry and shock metamorphism of Yamato 984028 lherzolitic shergottite
Petrography,mineral chemistry and shock metamorphism of Yamato 984028 lherzolitic shergottite作者机构:Key Laboratory of the Earth's Deep Interior Institute of Geology and Geophysics Chinese Academy of Sciences Beijing 100029 China Graduate University of Chinese Academy of Sciences Beijing 100049 China
出 版 物:《Chinese Science Bulletin》 (中国科学通报)
年 卷 期:2011年第56卷第15期
页 面:1579-1587页
核心收录:
学科分类:0709[理学-地质学] 070901[理学-矿物学、岩石学、矿床学] 07[理学]
主 题:矿物岩石学 矿物化学 变质作用 二氧化钛 激波诱导 撞击过程 陆地表面 压力淬火
摘 要:Y984028 is a new lherzolitic shergottite,consisting of poikilitic and non-poikilitic *** mafic silicates are FeO-poor,and the chromite is TiO 2-poor in the poikilitic lithology compared to the grains in the non-poikilitic *** meteorite shares similarmineral petrography andmineral chemistry with GRV 99027,but is not paired with the latter because of their different shock-induced features.Y984028 was severely shocked and experienced no significant thermal metamorphism after the main impact ***,Y984028 serves as a probe for the study of meteorite impact processes on terrestrial *** melt veins in Y984028 are characterized by the absence of any high-pressure polymorphs,the presence of abundant smallmineral fragments,and the prevailing granulation textures of olivine and *** features are consistent with adiabatic melting during the release of shock-induced high-pressure and quenching at ambient pressure.