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large decrease » marked decrease (Expand Search), large increases (Expand Search), large degree (Expand Search)
case increased » cases increased (Expand Search), care increased (Expand Search), causes increased (Expand Search)
b large » _ large (Expand Search), i large (Expand Search), _ larger (Expand Search)
a large » _ large (Expand Search)
_ case » a case (Expand Search)
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Sampling mutant’s fitness from the Gaussian.
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
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
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
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
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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