Abstract:Dendrite, a typical geological pattern, is developed along the bedding plane in limestone and dolomite strata in Jinzigou area, Zhoukoudian, Beijing, China, with a self-similar dendritic morphology. In order to reveal the dynamic mechanism of its formation, the diffusion-limited aggregation method, a model of fractal growth, was selected to simulate the microscopic dynamic mechanism of its formation. Take an L × L square lattice, with L = 200 lattices, 20,000 particles, and L = 250 lattices, 30,000 particles, … Show more
“…The paper authored by N. Liu, Y. He, S. Xu, L. Xiong, Y. Wei, J. Li, P. Li, and Q. Gong presents a dendrite developed along the bedding plane in limestone and dolomite strata in Zhoukoudian, Beijing city [12], where the formation's dynamic mechanism was simulated on the diffusion-limited aggregation method on a model of fractal growth.…”
The 9th national conference on applied geochemistry in China will be held in Chengdu, Sichuan province, in October 2023, hosted by the committee of applied geochemistry, the Chinese Society for Mineralogy, Petrology and Geochemistry (CSMPG) [...]
“…The paper authored by N. Liu, Y. He, S. Xu, L. Xiong, Y. Wei, J. Li, P. Li, and Q. Gong presents a dendrite developed along the bedding plane in limestone and dolomite strata in Zhoukoudian, Beijing city [12], where the formation's dynamic mechanism was simulated on the diffusion-limited aggregation method on a model of fractal growth.…”
The 9th national conference on applied geochemistry in China will be held in Chengdu, Sichuan province, in October 2023, hosted by the committee of applied geochemistry, the Chinese Society for Mineralogy, Petrology and Geochemistry (CSMPG) [...]
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