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首页> 外文期刊>Journal of geophysical research. Planets >Physical Properties of Basalt Ejecta Boulders at Lonar Crater, India: Insights Into the Target Heterogeneity and Impact Spallation Processes in Basalt With Application to Mars
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Physical Properties of Basalt Ejecta Boulders at Lonar Crater, India: Insights Into the Target Heterogeneity and Impact Spallation Processes in Basalt With Application to Mars

机译:玄武岩火山口玄武岩博尔德的物理性质:玄武岩中目标异质性和冲击脱落过程的见解,应用于火星

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摘要

The 1.88-km-diameter Lonar crater emplaced in the Deccan basalt is an excellent terrestrial analog of bowl-shaped impact craters on Mars. It contains a pristine ejecta blanket with abundant basalt boulders. We measured the density, porosity, P and S wave velocities and attenuation, magnetic susceptibility, uniaxial compressive strength, and tensile strength of 313 core specimens from 65 basalt ejecta boulders. Using these values, we quantified the gross physical properties of preimpact target and applied them in the cratering equations and estimated the spall plate dimensions and ejection distances. The impact of 35-m-radius projectile with 20 km/s velocity on the basaltic target with 77.2-MPa dynamic tensile strength, 4,163 m/s P wave velocity, and 2.56 g/cm~3 density gives a spall thickness range (0.2 to 9.7 m) similar to the observed boulder sizes at Lonar crater. Because aqueous weathering and vesicularity are present in the target, the Lonar impact produced smaller spall sizes than those expected from a massive basalt target. We also measured the ejecta boulder sizes and shapes around a fresh impact crater (of similar size and target to Lonar) in Arcadia Planitia on Mars and calculated the spall thicknesses. The low-velocity impact (5.5 km/s) of 50-m-radius projectile on the target similar to Lonar basalt gives a spall thickness range (1 to 25 m) similar to the observed boulder sizes at the Martian impact crater. The impact craters of similar sizes and targets on Earth and Mars produced different spall boulder size distributions reflecting the distinct impact conditions on these planets.
机译:位于德干玄武岩中的直径1.88公里的Lonar陨石坑是火星上碗状撞击坑的一个极好的地球模拟物。它包含一个原始的喷出物覆盖层,带有大量玄武岩巨石。我们测量了来自65块玄武岩抛石的313个岩芯样品的密度、孔隙度、P波和S波速度以及衰减、磁化率、单轴抗压强度和抗拉强度。利用这些数值,我们量化了撞击前目标的总体物理特性,并将其应用于弹坑方程中,估算了层裂板的尺寸和弹射距离。以20 km/s速度发射的35 m半径弹丸对玄武岩目标的冲击,其动态抗拉强度为77.2 MPa,P波速度为4163 m/s,密度为2.56 g/cm~3,产生的层裂厚度范围(0.2至9.7 m)与在Lonar陨石坑观察到的巨砾大小相似。由于靶标中存在水风化和气泡,Lonar撞击产生的层裂尺寸小于大块玄武岩靶标的预期尺寸。我们还测量了火星上阿卡迪亚平原一个新的撞击坑(大小和目标与Lonar相似)周围喷射物巨石的大小和形状,并计算了层裂厚度。50米半径的弹丸对目标的低速撞击(5.5千米/秒)类似于Lonar玄武岩,产生的层裂厚度范围(1至25米)类似于在火星撞击坑观察到的巨砾大小。地球和火星上大小和目标相似的撞击坑产生了不同的层裂巨石大小分布,反映了这些行星上不同的撞击条件。

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