Collaborative Research: Geomagnetic Field as Recorded in the Mount Erebus Volcanic Province: Key to Field Structure at High Southern Latitudes

该奖项由极地方案办公室南极地质和地球物理方案提供，支持一个调查过去500万年地球磁场的项目，以测试地球地磁发电机的模型。古地磁数据(从岩石中获得的古代地磁场的方向)在地球的各种地球物理研究中发挥着重要作用，包括板块构造重建、磁性地层学和研究古代地磁场的行为(称为古地磁)。在过去四十年中，许多古地磁学研究中的关键假设是，古地磁场的平均方向对应于由地心轴向偶极子(GAD)(类似于地球中心的条形磁铁)产生的方向，并且古倾角(岩石磁方向的倾角)提供了足够准确的数据，使其能够用于板块重建。最近对时间平均场基本数据模型的重新审查表明，现有数据库中最明显的缺陷是缺乏来自高纬度的高质量数据，包括古强度信息。该项目将在山上合适的地点进行采样和实验室计划。埃里巴斯火山省(南极洲)将从南部高纬度地区提供高质量的数据，这些数据对于加强对时间平均场及其长期变化的了解至关重要。

This award, provided by the Antarctic Geology and Geophysics Program of the Office of Polar Programs, supports a project to investigate Earth's magnetic field over the past 5 million years in order to test models of Earth's geomagnetic dynamo. Paleomagnetic data (directions of ancient geomagnetic fields obtained from rocks) play an important role in a variety of geophysical studies of the Earth, including plate tectonic reconstructions, magnetostratigraphy, and studies of the behavior of the ancient geomagnetic field (which is called paleo-geomagnetism). Over the past four decades the key assumption in many paleomagnetic studies has been that the average direction of the paleomagnetic field corresponds to one that would have been produced by a geocentric axial dipole (GAD) (analogous to a bar magnet at the center of the Earth), and that paleoinclinations (the dip of magnetic directions from rocks) provide data of sufficient accuracy to enable their use in plate reconstructions. A recent re-examination of the fundamental data underlying models of the time averaged field has shown that the most glaring deficiency in the existing data base is a dearth of high quality data, including paleointensity information, from high latitudes. This project will undertake a sampling and laboratory program on suitable sites from the Mt. Erebus Volcanic Province (Antarctica) that will produce the quality data from high southern latitudes that are essential to an enhanced understanding of the time averaged field and its long term variations.