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Shock-thermal history of Kavarpura IVA iron: Evidences from microtextures and nickel profiling

机译:Kavarpura IVA铁的冲击热历史:来自微观组织和镍轮廓的证据

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摘要

We classify Kavarpura iron (fell in August, 2006, in Rajasthan, India), an inclusion-free member of high-Ni IVA group. Widmanstatten pattern and finger-cellular plessites textures characteristic of IVA group are present in Kavarpura. Symmetric and asymmetric textural zoning within the cloudy taenite and plessite refer to long term martensitisation process with mean metallographic cooling rate of 200 degrees C/Ma. Imprints of variable shock pressure domains (Neumann bands and shock hatched epsilon kamacite) suggest alteration by up to 600 kb shock pressure. Degeneration of cellular plessites, bending of finger plessites and plastic flowage of taenites bear textural evidences corresponding to post-shock annealing which is further confirmed by Ni profiles across the cloudy taenites and plessites under high shock pressure domains. Based on microtextural evidences and Ni profiling, we suggest Kavarpura had cooled at steady state and subsequently suffered multiple impacts. (C) 2015 Elsevier Ltd. All rights reserved.
机译:我们将Kavarpura铁分类(于2006年8月在印度拉贾斯坦邦降落),它是高Ni IVA组的无杂质成员。卡瓦普拉(Kavarpura)中存在IVA基团特有的Widmanstatten图案和手指细胞的硅藻土质地。浑浊的钙钛矿和闪锌矿中对称和不对称的组织区划是指长期的马氏体化过程,平均金相冷却速率为200摄氏度/马来。可变的冲击压力域(Neumann谱带和带有冲击影线的epsilon kamacite)的压印表明,变化高达600 kb。蜂窝状磷灰石的变性,手指状磷灰石的弯曲和钛矿的塑性流动具有与冲击后退火相对应的组织证据,这进一步被高冲击压力域下横跨多云的钛矿和磷灰石的Ni分布所证实。根据微观组织证据和镍轮廓分析,我们建议卡瓦普拉(Kavarpura)在稳态下冷却,随后遭受多次冲击。 (C)2015 Elsevier Ltd.保留所有权利。

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