M A Kessler1, B T Werner

  • 1Complex Systems Laboratory, Cecil and Ida Green Institute of Geophysics and Planetary Physics, University of California, San Diego, La Jolla, CA 92093, USA. mkessler@es.ucsc.edu

Science (New York, N.Y.)
|January 18, 2003
PubMed
概括

在寒冷的环境中,自组织的石头和土壤模式源于结解周期. 这些循环产生反循环,将材料分类并移动石头,形成明显的圆形,多边形和条纹景观.

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