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首页> 外文期刊>Journal of geophysical research. Planets >A new global database of Mars impact craters ≥1 km: 2. Global crater properties and regional variations of the simple-to-complex transition diameter
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A new global database of Mars impact craters ≥1 km: 2. Global crater properties and regional variations of the simple-to-complex transition diameter

机译:≥1 km的火星撞击坑全球数据库:2.陨石坑的全球性质和简单到复杂过渡直径的区域变化

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摘要

We have generated a new, 384,343-entry global crater database of Mars, statistically complete for craters with diameters D ≥ 1 km. In this release, the database contains detailed morphologic and morphometric data for craters D ≥ 3 km (future releases will extend these to smaller diameters). With detailed topographic data for the largest crater database to-date, we analyzed crater depth-to-diameter ratios for simple and complex morphologies across various terrains and for the planet as a whole and investigated the simple-to-complex morphology transition. Our results are similar to those in the published literature, but we found a substantial terrain dependence of the simple-to-complex transition that occurs at ~11-km-diameter craters at high latitudes. This suggests a model that requires melting of volatiles during high-latitude crater formation that fill the crater during the modification phase but will still support the simple morphology to larger diameters. We also use this database to reexamine previously observed distributions and patterns to show its fidelity and to further explore other global relationships of fresh craters, those with central peaks, pits, and summit pits. We present the global distribution of craters with different types of ejecta and morphometric properties. Overall, this database is shown to be comparable to previous databases where there is overlap and to be useful in extending prior work into new regimes.
机译:我们已经生成了一个新的384343个条目的火星全球陨石坑数据库,该数据库在直径D≥1 km的陨石坑上具有统计意义。在此版本中,数据库包含D≥3 km的环形山的详细形态学和形态计量学数据(未来的版本会将其扩展到较小的直径)。借助迄今为止最大的陨石坑数据库的详细地形数据,我们分析了各种地形以及整个星球的陨石坑深度与直径之比,并研究了从单纯到复杂的形态转变。我们的结果与已发表的文献中的结果相似,但是我们发现在高纬度的直径约11公里的陨石坑中,发生了从简单到复杂的过渡过程,这在很大程度上取决于地形。这表明需要一个模型,该模型需要在高纬度火山口形成过程中挥发物熔化,并在改性阶段填充火山口,但仍将支持较大直径的简单形态。我们还使用该数据库重新检查以前观察到的分布和模式,以显示其保真度,并进一步探索新鲜火山口,具有中心峰,深坑和山顶深坑的其他全球关系。我们介绍了具有不同类型的喷射和形态特征的火山口的全球分布。总体而言,该数据库可证明与以前的数据库具有可比性,因为以前的数据库存在重叠并且在将先前的工作扩展到新制度方面很有用。

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