首页> 外文期刊>Meteoritics & planetary science >Shock-metamorphic petrography and microRaman spectroscopy of quartz in upper impactite interval, ICDP drill core LB-07A, Bosumtwi impact crater, Ghana
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Shock-metamorphic petrography and microRaman spectroscopy of quartz in upper impactite interval, ICDP drill core LB-07A, Bosumtwi impact crater, Ghana

机译:上部撞击岩层段中石英的变质岩石学和显微拉曼光谱,ICDP钻芯LB-07A,Bosumtwi撞击坑,加纳

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摘要

Standard and universal stage optical microscope and microRaman spectroscopic examination of quartz from the upper impactite interval of the International Continental Scientific Drilling Program (ICDP) Lake Bosumtwi crater drill core LB-07A demonstrates widespread but heterogeneous evidence of shock metamorphism. In the upper impactite, which comprises interbedded polymict lithic breccia and suevite from a drilling depth of 333.4-415.7 m, quartz occurs as a major component within metasedimentary lithic clasts and as abundant, isolated, single-crystal grains within matrix. The noted quartz shock-metamorphic features include phenomena related to a) deformation, such as abundant planar microstructures, grain mosaicism, and reduced birefringence; b) phase transformations, such as rare diaplectic quartz glass and very rare coesite; c) melting, such as isolated, colorless to dark, glassy and devitrified vesicular melt grains; and d) secondary, post-shock features such as abundant, variable decoration of planar microstructures and patchy grain toasting. Common to abundant planar deformation features (PDFs) in quartz are dominated by omega {10 (1) over bar3}-equivalent crystallographic planes, although significant percentages of pi {10 (1) over bar2} and other higher index orientations also occur; notably, c(0001) planes are rare. Significantly, the quartz PDF orientations match most closely those reported elsewhere from strongly shocked, crystalline-target impactites. Barometry estimates based on quartz alteration in the upper impactite indicate that shock pressures in excess of 20 GPa were widely reached; pressures exceeding 40-45 GPa were more rare. The relatively high abundances of decorated planar microstructures and grain toasting in shocked quartz, together with the nature and distribution of melt within suevite, suggest a water- or volatile-rich target for the Bosumtwi impact event.
机译:从国际大陆科学钻探计划(ICDP)博苏姆特维火山口火山口岩心LB-07A的上部撞击岩层中进行的石英的标准和通用光学显微镜以及显微拉曼光谱检查,证明了冲击变质作用的广泛但异质证据。在上层冲积岩中,钻进深度为333.4-415.7 m,包括层状多晶岩片角砾岩和钠铝榴石,石英是准沉积岩屑碎屑中的主要成分,而在基质中则是丰富,孤立的单晶晶粒。著名的石英冲击变质特征包括与a)变形有关的现象,例如丰富的平面微结构,晶粒镶嵌和双折射降低; b)相变,例如稀有的双折石英玻璃和非常稀有的堇青石; c)熔化,如孤立的,无色至深色,玻璃状和失透的水泡状熔化颗粒; d)震荡后的次要特征,例如平面微结构的丰富可变装饰和不规则的谷物烘烤。石英中丰富的平面形变特征(PDF)的共同点是在bar3}等效晶体平面上的Ω{10(1)),尽管也发生了显着百分比的pi {10(1)over bar2}和其他更高折射率的取向;值得注意的是,c(0001)平面很少见。值得注意的是,石英PDF方向与其他地方从强烈震动的晶体目标撞击矿中报告的方向最接近。基于上层撞击岩中石英蚀变的气压计估计表明,广泛达到了超过20 GPa的冲击压力。压力超过40-45 GPa的情况更为罕见。冲击石英中装饰的平面微观结构和晶粒烘烤的相对较高的丰度,以及苏维石内部熔体的性质和分布,都为Bosumtwi撞击事件提供了富含水或挥发性的目标。

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