台湾のチェルンプー断層圏の掘削孔配列で観測された同流現象
Kuo-Fong Ma1, Yen-Yu Lin, Shiann-Jong Lee
1Department of Earth Sciences, and Institute of Geophysics, National Central University, Taiwan, Republic of China. fong@ncu.edu.tw
まとめ
研究者らは台湾で地震を観測した.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 地震学 地震学とは
- ロック・メカニクス ロック・メカニクス
背景:
- 剪定障害は,断層地帯における地震プロセスを支配する.
- 流体の高圧は岩石の破裂を引き起こしますが,断層地帯の直接観測は欠けています.
研究 の 目的:
- 断層地帯における高流体圧によって引き起こされる可能性がある地震現象を調査する.
- 地震が活発な地域における天然水力断裂のメカニズムを理解する.
主な方法:
- 台湾のチェルンプー断層地帯からの掘削孔配列地震データの分析.
- 地震発生源メカニズムのモデリング.
主要な成果:
- メインスリップゾーンの下の液体豊富なゾーンで観測された小規模な地震 (I型) 発生.
- イベントをモデル化して,同otropic, nonshear ソースメカニズムを持つ.
- 自然な水力断裂を潜在的に表すものとして解釈された出来事.
結論:
- 断層地帯における流体圧力による岩石破裂の直接観察を提供した.
- 自然な水力断層の形成と流体特性の関連した地震現象.
- これらの自然過程と人工水力破裂の類似性を示唆した.
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