Structure and Dynamics of the Porcupine Magma-Poor Continental Margin from new Ocean Bottom Seismometer Data

该项目将包括使用全新的海底地震仪数据和协同定位的工业多通道地震数据。该项目将完成豪猪盆地的地图绘制，以揭示裂谷的对称性，以及大陆分裂期间水进入地幔的程度。豪猪盆地是岩浆贫乏裂谷的典型。项目的一部分将与加利西亚（西班牙）的数据进行比较，加利西亚是伯明翰提议的IODP钻井地点，以及伯明翰领导的NSF/NERC 3D地震成像计划，这将使我们能够测试关于岩浆贫乏裂缝的动力学和时间演化的假设。

The project will include the use of brand-new ocean bottom seismometer data and co-located industrial multi-channel seismic data. This project will complete the mapping of the Porcupine Basin an exemplar of a magma-poor rift, to reveal the symmetry of rifting, and degree of water ingress to the mantle during continental break-up. Part of the project will be comparing with data from Galicia (Spain), the site of Birmingham-proposed IODP drilling and a Birmingham-led NSF/NERC 3D seismic imaging programme this will allow us to test hypotheses for the dynamics and temporal evolution of magma-poor rifts.