An Automatic Marine Seismic Monitoring and Recording Device

J. T. Thomson, W. Schneider
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引用次数: 43

Abstract

An automatic marine seismic monitoring and recording instrument of recoverable design is discussed. The instrument is capable of measuring three components of earth motion and water pressure waves and is intended for use on the ocean bottom at depths to 10,000 feet. Most previous seismic data has been recorded at land-based stations and the collection of ocean-floor seismic information will materially add to the knowledge of origin and propagation phenomena. Data are recorded on magnetic tape in digital form. Seismic motion is recorded in the 1-10 cps band with a sensitivity below 0.1 millimicron of earth movement. Pressure information is recorded over the same bandwidth with comparable sensitivity. Up to eight hours of data can be recorded on a programmed cycle during each implanting of the instrument. Initial sea tests of the instrument indicate that the unit functioned as desired. Several events recorded during the test period appeared to give valid seismic information. One of these events is described. Simultaneous recording of pressure and velocity is expected to enhance detection capability. It is planned in a future program to collect additional seismic information in much deeper waters and at sites chosen for maximum quality data return. The data will represent the first extensive effort to collect and analyze three-component seismic (plus pressure) information at great ocean depths.
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一种海洋地震自动监测记录装置
讨论了一种可回收式海洋地震自动监测记录仪的设计。该仪器能够测量地球运动和水压波的三个组成部分,旨在用于10000英尺深的海底。以前的大多数地震资料都是在陆基台站记录的,海底地震资料的收集将大大增加对地震起源和传播现象的认识。数据以数字形式记录在磁带上。地震运动记录在1- 10cps波段,灵敏度低于0.1微米的地球运动。在相同的带宽上以相当的灵敏度记录压力信息。在每次植入仪器期间,可在编程周期内记录长达8小时的数据。仪器的初步海上试验表明,该装置按预期工作。在测试期间记录的几个事件似乎提供了有效的地震信息。描述了其中一个事件。同时记录压力和速度有望提高探测能力。在未来的项目中,计划在更深的水域和选择的地点收集更多的地震信息,以获得最高质量的数据返回。这些数据将是在大洋深处收集和分析三分量地震(加压力)信息的首次广泛努力。
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