An integrated approach to understanding the magnetic signal in sediments and its application to sedimentary unconformity 5

Линиите свързват координатора с партньорите. За проекти отпреди 2014 г. CORDIS не винаги дава точни координати. Тези точки са на ниво град или държава.

Накратко на български

Цел на проекта

Because rock magnetic methods are comparatively rapid, they are increasingly applied in Earth Sciences providmg a high resolution tool to analyse past environmental and climatic changes recorded in geological materials. For a scientifically correct interpretation, however, potentially biasing diagenetic effects on the (paleo)magnetic signal must be completely understood. The underlying proposal intends to provide an in-depth insight of these diagenetic effects by combing two promising recent approaches, one put forward by me, the other proposed by the envisaged host laboratory. Part I of the work involves the synthesis of these two approaches so as to establish a sound basis for their application to sedimentary unconformities which potentially cause a dramatic, yet unknown, diagenetic alteration of the magnetic signal (part II). The outcome of the research will significantly enhance rock magnetism as an interdisciplinary tool for the analysis of paleo-environment and paleoclimate, including the retrieval of true geomagnetic information stored in the paleomagnetic signal.

Оригинален текст от CORDIS (на английски).

Участници

• Rijksuniversiteit Utrecht · UtrechtКоординаторНидерландия
• Not availableНиво градГермания

Връзки

• Виж в CORDIS