Skip to main content
European Commission logo
English English
CORDIS - EU research results
CORDIS
Content archived on 2024-05-14

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

Objective



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.

Call for proposal

Data not available

Coordinator

Rijksuniversiteit Utrecht
EU contribution
No data
Address
17,Budapestlaan 17
3584 CD Utrecht
Netherlands

See on map

Total cost
No data

Participants (1)