在胡安·德福卡中洋山脊上,地震引起的水热系统的变化
1School of Oceanography, University of Washington, Seattle 98195-7940, USA. johnson@ocean.washington.edu
Nature
|September 23, 2000
概括
地震群可以改变深海的热水喷口. 构造活动导致了通风流体温度和沿胡安德富卡山脊段输出的显著,持续增加.
科学领域:
- 海洋地质学和地球物理学
- 海洋学 海洋学 海洋学
- 热水系统是热水系统.
背景情况:
- 众所周知,中海山脊上的热水喷口会对地震干扰做出反应,通常与海底火山活动有关.
- 以前的观测集中在与火山有关的地震事件上,并没有研究对非磁性,构造事件的反应.
研究的目的:
- 为了研究水热风口系统对非磁性,构造性地震群的反应.
- 为了测量风口流体温度和输出在构造性地震活动后的变化.
主要方法:
- 在1999年6月在胡安德福卡山脊的几个热水喷口进行了温度测量.
- 在地震前,地震期间和地震后监测风口液体温度,地震群是明显的构造起源.
- 在长时间内评估流体输出的变化.
主要成果:
- 在最初的地震4-11天后,通风流体温度开始上升,在稳定在更高的值之前,振荡大约一个月.
- 观察到液体输出量增加了十倍,持续至少80天.
- 热反应沿着整个脊段延伸.
结论:
- 温和的构造活动可以触发水热系统中显著的,整个部分的热反应.
- 这些发现引发了有关多余热量和流体来源及其对通风生态系统的影响的问题.
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