Seismicological Components of the MELT Experiment on the Southern East Pacific Rise

东南太平洋海隆 MELT 实验的地震学成分

• 批准号: 9402991
• 负责人: Sean Solomon
• 金额: $ 11万
• 依托单位: Carnegie Institution of Washington
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 1996
• 资助国家: 美国
• 起止时间: 1996-06-01 至 2000-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=9402991&HistoricalAwards=false
• 关键词: Seismicological; Components; MELT; Experiment; Southern

This experiment is designed to provide direct observational constraints on the distribution of melt and the pattern of upwelling beneath a mid-ocean ridge. Studies of electromagnetic and seismic wave propaation in the mentle with arrays of ocean- bottom instruments will furnish measurements that can be inverted to find horizontal and vertical variations in velocity and conductivity structure that can be used to test theoretical models of flow. An array of 47 ocean-bottom seismometers will be deployed for six months on the East Pacific Rise at about 17 degrees south to record teleseismic and regional earthquake sources. P and S waves, as well as other bady wave phases and Love and Rayleigh surface waves recorded by the array will be used to probe lateral variations in mantle structure to a depth of 100 to 200 km and out to several hundred km from the ridge axis. The mail goal is to establish whether there is a narrow region of high melt concentration and low seismic velocities directly beneath the ridge axis and to map its vertical and horizontal extent. Another goal is to constrain the pattern of upwelling.

该实验的目的是为融化的分布和洋中脊下方的上升流模式提供直接的观测约束。 利用海底仪器阵列对海底电磁波和地震波传播的研究将提供测量结果，这些测量结果可以反演以发现速度和电导率结构的水平和垂直变化，从而可用于测试流动的理论模型。 一组由 47 个海底地震仪组成的阵列将在南​​纬 17 度左右的东太平洋隆起部署为期六个月，以记录远震和区域地震源。 P波和S波，以及阵列记录的其他巴迪波相位以及洛夫和瑞利表面波将用于探测地幔结构的横向变化，深度可达100至200公里，距脊轴数百公里。 主要目标是确定山脊轴正下方是否存在高熔体浓度和低地震速度的狭窄区域，并绘制其垂直和水平范围。 另一个目标是限制上升流的模式。