産業技術総合研究所(産総研)
地質調査総合センター(地調)
参加自由ですので,どなたでもぜひ議論にご参加下さい.
なお,準備や連絡の都合もありますので,所外(第7事業所外)から参加を希望される方は予め世話人までお知らせ下さい.(突然の予定変更などは原則として所内にしか通知いたしませんので.)
火山談話会では,講演者を随時募集しております.
談話会で話題提供したい方(自薦・他薦問わず)がいらっしゃいましたら,
お気軽に世話人(下記)までお声掛け下さい.所外の方も歓迎です.
We review the evolution of the A.D. 2000 Miyakejima caldera, with two concentric ring faults at earlier collapsing stages, and erosion of its wall, accumulating debris on the floor, at later collapsing stages. While St/Dt and Ss/Ds show a similar increase at initial stages, when Ss/Ds~0.33 the Ss/Ds becomes significantly different from St/Dt: while continuous caldera subsidence monotonically increases Ss/Ds, the erosion of the wall and the filling of the floor decrease St/Dt.
This evolution finds close similarities with recent caldera collapses such as Katmai (1912), Pinatubo (1991) and Dolomieu (2007). Analogue experiments mimic the observed variation, evolving from a depression controlled by the activity of the double-ring faults to that controlled by the erosion of the wall and sedimentation at the floor.
These natural and modeling results show that the control on the shape of mature calderas (Ss/Ds>0.07) and approaching Ss/Ds = 0.3-0.4 passes from a mainly structural to a mainly erosional control. Both St/Dt and Ss/Ds are needed to describe the evolution of a collapse and the processes accompanying it. Evaluating St/Dt and Ss/Ds allows proper description of the precise evolutionary stage of a caldera and of the relative importance of the structural and erosional processes and allows making semi-quantitative comparisons between evolutionary stages.
講演者は随時募集中です!!
これまでに行なわれた講演のリストは,
こちら(http://staff.aist.go.jp/a.tomiya/volc_conf_b.html)をご覧下さい.
火山活動研究推進部会談話会世話人:
大石 雅之(マグマ活動RG) E-mail: ooishi-m@ (@の後ろに "aist.go.jp" をつけてください)
下司 信夫(火山活動RG) E-mail: geshi-nob@ (@の後ろに "aist.go.jp" をつけてください)