关于苏门答腊,印度尼西亚苏丹湾西部的地震性的一些注意事项,与后弓推进的潜力有关
S Widiyantoro1,2, P Supendi3,4, N Rawlinson5
1Global Geophysics Research Group, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, 40132, Indonesia.
Scientific reports
|June 7, 2024
概括
这项研究调查了苏门答腊的反弧推力断层,发现它们并不普遍. 可能存在间歇性断层,影响印尼地震危险评估.
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 地震学 地震学
背景情况:
- 已知后弓推力断层位于东部的桑达弧 (从弗洛雷斯到爪).
- 它们在苏门答腊 (西桑达弧) 的存在仍未得到证实.
- 了解这些结构对于地震危险评估至关重要.
研究的目的:
- 为了确定苏门答腊背弧推力断层的存在和程度.
- 为了分析苏门答腊后弧区域的地震性模式.
- 为了为印尼的地震危险绘制提供信息.
主要方法:
- 分析区域地震数据 (印度尼西亚的BMKG).
- 对全球地震目录 (ISC,USGS) 的检查.
- 解释地震数据以确定故障机制.
主要成果:
- 与苏门答腊东部的达弧相比,后弧推力在苏门答腊并没有得到广泛发展.
- 斜俯冲和大苏门答腊断层可能适应压力.
- 一个浸泡的地震带,与板块沉降相反,表明间歇性的后弓推力.
结论:
- 在苏门答腊可能存在空间间歇的反弧推力断层.
- 这些断层可能会影响地震危险评估.
- 需要进一步考虑印度尼西亚的国家地震危险地图.
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