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通过计算裂缝来解读行星表面。

Decoding planetary surfaces by counting cracks.

作者信息

Silver S, Regős K, Jerolmack D J, Domokos G

机构信息

Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, PA 19104.

Department of Morphology and Geometric Modeling, Budapest University of Technology and Economics, Budapest 1111, Hungary.

出版信息

Proc Natl Acad Sci U S A. 2025 Mar 11;122(10):e2411738122. doi: 10.1073/pnas.2411738122. Epub 2025 Mar 4.

Abstract

Planets are often covered with thin cracked shells. From mud films to lithospheres of rock or ice, fracture networks form two-dimensional (2D) tessellations of convex polygons whose geometry encodes their genesis. Here, we chart the geometry of 2D fracture mosaics across the solar system, and decode their formative conditions using a new dynamical crack model. We show that mosaics can be projected onto a Symbolic Ternary Diagram, where the relative proportions of "T," "X," and "Y" junctions are uniquely related to contributions from distinct modes of fracture. Most planetary mosaics cluster in a region associated with hierarchical fracture networks, where sequential cracking favors formation of T junctions. Exceptions to this rule may betray the presence of water. Europa's fracture networks stand apart due to the predominance of X junctions; this is a special feature of ice, where healing of cracks by refreezing of water allows new fractures to overprint older ones. Several fracture networks on Mars appear as outliers due to the high proportion of Y junctions. These patterns-previously interpreted as ancient mudcracks and frozen polar terrain, based on geological evidence-are consistent with the twisting of crack junctions by cyclic volume change. Our findings suggest that counting cracks could aid in the identification of other water-influenced planetary environments.

摘要

行星表面通常覆盖着薄薄的破裂外壳。从泥膜到岩石或冰层的岩石圈,断裂网络形成了凸多边形的二维(2D)镶嵌图案,其几何形状记录了它们的成因。在这里,我们绘制了整个太阳系二维断裂镶嵌图案的几何形状,并使用一种新的动态裂纹模型来解读它们的形成条件。我们表明,镶嵌图案可以投影到一个符号三元图上,其中 “T”、“X” 和 “Y” 型节点的相对比例与不同断裂模式的贡献有着独特的关联。大多数行星镶嵌图案聚集在一个与分层断裂网络相关的区域,在那里连续的开裂有利于T型节点的形成。这条规则的例外情况可能意味着水的存在。木卫二的断裂网络与众不同,因为X型节点占主导地位;这是冰的一个特殊特征,水重新冻结使裂缝愈合,从而使新的裂缝能够叠加在旧的裂缝之上。火星上的几个断裂网络由于Y型节点的比例较高而显得异常。基于地质证据,这些模式以前被解释为古代泥裂和冻结的极地地形,它们与周期性体积变化导致的裂缝节点扭曲是一致的。我们的研究结果表明,统计裂缝数量可能有助于识别其他受水影响的行星环境。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e6a3/11912463/cfcfe100d27f/pnas.2411738122fig01.jpg

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