@article{oai:kumadai.repo.nii.ac.jp:00029880,
 author = {宮縁, 育夫 and Miyabuchi, Yasuo and 星住, 英夫 and Hoshizumi, Hideo and 宮縁, 育夫 and Miyabuchi, Yasuo and 星住, 英夫 and Hoshizumi, Hideo},
 issue = {4},
 journal = {火山},
 month = {},
 note = {application/pdf, 論文(Article), The Asosan core (JMA-V40) was drilled at a site 1.2km WSW of Nakadake crater, Aso Volcano in 2009. The core consists of the following nine units: 1)alternating beds of ash-fall deposits and buried soil layers (0-3.49m in depth); 2)alternating beds of ash including Nakadake N2 scoria (N2S; 1.5ka) (3.49-4.46m); 3)scoria-fall deposits from Kishimadake scoria cone (4ka; 4.46-9.00m); 4)a basaltic andesite lava (lava 1, 9.00-23.72m); 5)alternating beds of ash, soils and lahar deposits including the Kikai Akahoya tephra (K-Ash; 7.3ka) (23.72-31.00m); 6)a basaltic andesite lava (lava 2, 31.00-76.11m); 7)lahar deposits (76.11-86.47m); 8)a basaltic andesite lava (lava 3, 86.47-91.64m); 9)lahar deposits (91.64-100.00m). The three lavas recognized in units 4, 6 and 8 are quite similar in lithofacies, petrography and major element composition (SiO2=52.1-53.4wt.%). This suggests that at least two compositionally homogeneous basaltic andesite lava flows were erupted from Nakadake Volcano around 8-5calka and another similar one erupted somewhat earlier, but still in Holocene time., https://www.jstage.jst.go.jp/article/kazan/58/4/58_KJ00008993028/_article/-char/ja/},
 pages = {543--550},
 title = {2009年気象庁阿蘇山ボーリングコアの層序},
 volume = {58},
 year = {2013},
 yomi = {ミヤブチ, ヤスオ and ホシズミ, ヒデオ and ミヤブチ, ヤスオ and ホシズミ, ヒデオ}
}