3D structure of the crust and upper mantle beneath Northern Fennoscandian shield

• Main Author: Silvennoinen, H. (Hanna)
• Other Authors: Kozlovskaya, E. (Elena), Kaikkonen, P. (Pertti)
• Format: Doctoral or Postdoctoral Thesis
• Language: English
• Published: University of Oulu 2015
• Subjects: Bouguer anomaly; Fennoscandia; P-wave velocity; controlled source seismic methods; crust; density modelling and inversion; receiver function; teleseismic tomography; upper mantle; Norway; Fennoscandian; Northern Finland; Lapland
• Online Access: http://urn.fi/urn:isbn:9789526210681

Abstract The crustal and upper mantle structures of the Shield on the regional scale were investigated using the data of the POLENET/LAPNET passive seismic array and the previously published models of active and passive seismic experiments in the study area. This area is centred in northern Finland and it extends to surrounding areas in Sweden, Norway and northwestern Russia. The bedrock there is mostly of the Archaean origin and the lithosphere of the region was reworked by two orogenies during Palaeoproterozoic. One of the results of the thesis was a new map of the Moho depth of the study area, for which new estimates of the crustal thickness were obtained using receiver function method and complemented by published results of receiver function studies and controlled source seismic profiles. The map differs from the previously published maps in two locations, where we found significant deepening of the Moho. The 3D structure of the upper mantle was studied using teleseismic traveltime tomography method. The resulting model shows high seismic velocities below three cratonic units of the study area, which may correspond to non-reworked fragments of cratonic lithosphere and a low velocity anomaly separating these cratonic units from each other. The regional scale studies were complemented by two smaller scale studies in upper crust level using combined interpretation of seismic profiling and gravity data. These studies were centred on Archaean Kuhmo Greenstone Belt in eastern Finland and central Lapland in northern Finland located in the crust reworked during Palaeoproterozoic. Both areas are considered as prospective ones for mineral exploration. Both studies demonstrate the advantage of gravity data inversion in studying 3D density structure of geologically interesting formations, when the Bouguer anomaly data is combined with a priori information from petrophysical and seismic datasets.