Fine-Scale Crustal Structure of the Kane Fracture Zone in 0-80 Million Year-Old Crust

这是一个项目，研究精细规模的构造， 凯恩断裂带从0到80米，作为对 板块运动这项工作将通过执行SeaMARC来完成 II剖面沿着断裂带的东、西翼。 轨道线将与断裂走向成一定角度 区域，以便从SeaMARC中获取最大信息 显像 还将使用深拖磁力计， 对出现在 断裂带的共轭肢。的主要产品 该研究将是一个确定的精细规模的限制， KFZ记录了板块运动的变化， 了解FZ响应是否/或在何种情况下 在两个RTI处同步和/或对称地发生。 的 还将开始工作，为审查全球 板块相互作用

This is a project to study the fine-scale tectonics of the Kane Fracture Zone from 0 to 80 my as a response to changes in plate motion. The work will be accomplished by performing SeaMARC II profiles along the east and west limbs of the fracture zone. Track lines will be run at an angle to the trend of the fracture zone in order to obtain maximum information from the SeaMARC imaging. A deep-towed magnetometer will also be used in order to provide age control on structuralfeatures that appear on conjugate limbs of the fracture zone. The principal products of the research will be a determination of the fine-scale limit at which the KFZ records changes in plate motion, an improved understanding of whether/or in what circumstances the FZ response occurred synchronously and/or symmetrically at the two RTIs. The work will also begin to provide a data base for examining Global plate interactions.