Late Quaternary Paleomagnetic Intensities and Secular Variation from Dated Lavas In Southern Europe

地磁强度可能是最不为人所知的 古地磁场的参数，出现之前， 约10 ka B.P.（ka = 1000 年; B. P.=现在之前）。 该奖项支持研究 古地磁强度和长期变化 过去9万年，记录在50多个过时的熔岩的 法国奥弗涅中央高地和类似的研究， 起源于意大利，年代约为130 ka B. P. 该研究将有助于对该病毒的矢量描述 晚第四纪地磁场，显著延长了 古地磁强度和方向的古地磁记录 在南欧，大约130 ka B. P.。 更全面地描述该领域， 了解地球发电机的过程， 存在

The geomagnetic intensity is probably the least well known parameter of the paleomagnetic field, prior to the appearance of baked archeological artifacts about 10 ka B.P. (ka = thousand years; B.P. = before present). This award supports studies of the paleomagnetic intensities and secular variation during the past 90 millennia, recorded in more than 50 dated lavas of the Massif Central, Auvergne, France, and similar studies of dated flows from Italy, whose ages extend to about 130 ka B.P. The study will contribute to the vector description of the late Quaternary geomagnetic field, extending significantly the archeomagnetic record of paleomagnetic intensities an directions in southern Europe to about 130 ka B.P. Such data are needed for a more complete description of the field and for a more thorough understanding of the geodynamo processes responsible for its existence.