一种用于深度地质物理调查的两种不同地震源交替拍摄的新方法
ChenGuang Liu1, JinZhong Fu1, QingFeng Hua1
1Key Laboratory of Marine Geology and Metallogeny, The First Institute of Oceanography, Ministry of Natural Resources, Qingdao, 266061, China.
Scientific reports
|June 19, 2023
概括
一种新的地质物理调查方法使用双重地震源,同时获取海面和海底数据. 这种创新方法提高了海上深海地震调查的效率和数据丰富性.
科学领域:
- 地质物理学 地质物理学
- 海洋地质学 海洋地质学
- 地震勘探的地震勘探工作
背景情况:
- 传统的地震调查在实现深度透和全面数据采集方面存在局限性.
- 印度洋的九十东是地球物理研究的关键区域.
研究的目的:
- 引入和评估一种用于比例双重地震源激发的新方法.
- 从海面和海底同时获取地震数据.
主要方法:
- 使用了两个不同的地震源:G炮阵列 (450英寸3容量,20-100赫兹) 和博尔特炮阵列 (6000英寸3容量,10-40赫兹).
- 采用480通道的地震流器和21个海底地震计 (OBS) 来接收信号.
- 在G枪和Bolt枪阵列之间实现了3:1的触发信号分配比.
主要成果:
- 成功生成了三种类型的地震配置文件:常规 (2公里透),深 (6公里透) 和主动源OBS (30公里透).
- 从多个接收器和来源同时采集数据.
结论:
- 这种新方法显著提高了离岸深海地震调查的效率.
- 提供更丰富的数据集,具有不同的透深度,用于增强地质解释.
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