穿越银河系的地质望远镜?

C. L. Kirkland, P. Sutton
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摘要

我们所处的位置是银河系相对内部的位置,这阻碍了我们了解银河系结构的能力。然而,通过对其他星系的天体物理观测以及光谱测量,我们得出了银河系的模型,它是一个设计宏伟的棒状旋臂星系,有两个或四个旋臂。目前的任何天体物理技术都无法通过银河系的平面进行观测。不过,也许地球地质学可以帮助我们解决目前观测恒星环境所无法解决的问题。在太阳系围绕银河中心运行的过程中,地球会看到不同的宇宙环境,这是太阳系轨道(240 千米/秒)快于旋臂密度波(210 千米/秒)的结果。具体地说,如果地球撞击记录或其代用物以某种隐秘的方式反映了当地太阳系引力场的扰动,那么地球就可能充当地质箭塔,产生一些有趣的影响。在此,我们探讨了银河系设计的各种模型,并通过我们星球内部的深层时间记录,将这些模型与一些人提出的作为撞击通量指标的地质代用指标进行了比较。锆石中的同位素特征与四臂螺旋模型在统计学上是一致的。然而,地球同位素记录与更复杂的银河系原子氢模型之间的对应关系甚至更好。
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A geological telescope through the galaxy?
We reside within a relatively interior position within the Milky Way galaxy which hinders our ability to understand its structure. Nonetheless, astrophysical observations of other galaxies in unison with spectroscopic measurements have produced a model for the Milky Way as a grand design, barred, spiral arm galaxy, with either two or four arms. Viewing through the plane of the Milky Way is not possible with any current astrophysical technique. However, perhaps terrestrial geology can help where current observations of our stellar environment cannot. During the orbit of our solar system around the galactic centre, Earth will have seen different cosmic surroundings, as a function of the solar system's orbit (240 km/s) that is faster than the spiral arm's density waves (210 km/s). Specifically, if the terrestrial impact record, or proxies for it, in some cryptic way reflect perturbations on the gravity field of the local solar system, then Earth may act as a geological orrery, with some interesting implications. Here we explore various models for the design of the Milky Way and compare these to geological proxies proposed by some as indicators for impact flux, through the deep time record within our planet. Isotope signatures in zircon are statistically coherent with a four-armed spiral model. However, even better correspondence is shown between the terrestrial isotopic record and more complex atomic hydrogen models of the galaxy.
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