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Characteristics in naturally and experimentally shocked chondrites: A clue to P-T conditions of impacted asteroids

机译:自然和实验冲击球粒陨石的特征:撞击小行星的PT条件的线索

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摘要

The aim of this study is to compare the experimentallyshock-induced features with those in naturally shocked chondrites andto test the feasibility of experimentally calibrating naturallyinduced features in shocked H- and L-chondrites. Samples of the Jilinchondrite (H5) were experimentally shock-loaded at the following peakpressures: 12, 27, 39, 53, 78, 83, 93 and 133 Gpa respectively.Chondritic melts were first obtained at P>78 Gpa and more than 60/100melting was achieved at P?133 GPa. No high-pressure phases wereobserved in any of the shocked samples, neither in the deformed norin the molten regions.
机译:本研究的目的是将实验激波诱导的特征与自然激波球粒陨石的特征进行比较,并测试实验校准激波 H 球粒陨石和 L 球粒陨石中自然诱导特征的可行性。吉林球粒陨石(H5)样品在以下峰值压力下进行了实验冲击载荷:分别为12、27、39、53、78、83、93和133 Gpa。首先在P>78 Gpa下获得软粒熔体,在P?133 GPa下实现了超过60/100的熔化。在任何冲击样品中均未观察到高压相,在变形和熔融区域均未观察到高压相。

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