Showing 1 - 15 results of 15 for search '(((( ((_ largest) OR (b large)) decrease ) OR ( a large decrease ))) OR ( _ case increased ))~', query time: 0.86s Refine Results
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    Sampling mutant’s fitness from the Gaussian. by Nikhil Sharma (571073)

    Published 2023
    “…(B) Increasing the <i>σ</i> from 0.1 to 1, the average fitness in the steady-state goes down for many graphs. …”
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    DataSheet1_Long-term change of the eruption activities of Sakurajima volcano, Japan, inferred from the fallout tephra deposits.PDF by Ayumu Nishihara (14173077)

    Published 2022
    “…Among them, Stage 2a (13–8 ka) produced the largest volume of tephra fallout deposits, suggesting that Sakurajima peaked in magma discharge during Stage 2a (2.9 km<sup>3</sup>/kyr) and then decreased rapidly toward Stage 2b (8–4.8 ka; 0.07 km<sup>3</sup>/kyr). …”
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    DataSheet3_Long-term change of the eruption activities of Sakurajima volcano, Japan, inferred from the fallout tephra deposits.PDF by Ayumu Nishihara (14173077)

    Published 2022
    “…Among them, Stage 2a (13–8 ka) produced the largest volume of tephra fallout deposits, suggesting that Sakurajima peaked in magma discharge during Stage 2a (2.9 km<sup>3</sup>/kyr) and then decreased rapidly toward Stage 2b (8–4.8 ka; 0.07 km<sup>3</sup>/kyr). …”
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    Table1_Long-term change of the eruption activities of Sakurajima volcano, Japan, inferred from the fallout tephra deposits.XLSX by Ayumu Nishihara (14173077)

    Published 2022
    “…Among them, Stage 2a (13–8 ka) produced the largest volume of tephra fallout deposits, suggesting that Sakurajima peaked in magma discharge during Stage 2a (2.9 km<sup>3</sup>/kyr) and then decreased rapidly toward Stage 2b (8–4.8 ka; 0.07 km<sup>3</sup>/kyr). …”
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    DataSheet2_Long-term change of the eruption activities of Sakurajima volcano, Japan, inferred from the fallout tephra deposits.PDF by Ayumu Nishihara (14173077)

    Published 2022
    “…Among them, Stage 2a (13–8 ka) produced the largest volume of tephra fallout deposits, suggesting that Sakurajima peaked in magma discharge during Stage 2a (2.9 km<sup>3</sup>/kyr) and then decreased rapidly toward Stage 2b (8–4.8 ka; 0.07 km<sup>3</sup>/kyr). …”
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