Implications on crustal structure from the South Finland Coastal (SOFIC) deep seismic sounding profile

• Main Authors: Tiira, Timo, Janik, Tomasz, Veikkolainen, Toni, Komminaho, Kari, Skrzynik, Tymon, Väkevä, Sakari, Heinonen, Aku
• Other Authors: Suomen ympäristökeskus, The Finnish Environment Institute
• Format: Article in Journal/Newspaper
• Language: English
• Published: The Geological Society of Finland 2023
• Subjects: seismology; Moho; reflection; profile; crust; earth's crust; lithosphere; deep sounding; tectonics; Precambrian; Fennoscandia; Finland; Southern Finland; seismologia; maankuori; litosfääri; syväluotaus; tektoniikka; prekambri; Fennoskandia; Suomi; Etelä-Suomi; Uusimaa
• Online Access: http://hdl.handle.net/10138/357489

We present results from a deep seismic sounding (DSS) experiment carried out along the southern coast of Finland in summer 2015. Data used in the survey derived from industrial blasts recorded by temporary project stations and permanent network stations. The western 220 km part of the 450 km long Southern Finland Coastal (SOFIC) profile runs along the Uusimaa belt (UB) in the 1.7–1.9 Ga Southern Finland subprovince (SFS) of the Svecofennian domain, while the 170 km part in the east crosses the 1.62–1.65 Ga Wiborg rapakivi batholith (WRB). The farthest 60 km cross a geologically diverse area consisting of supracrustal rocks and granitoids of the Saimaa area (SA), an eastern extension of the SFS. Our results show that the Moho boundary depth varies significantly, from ca. 52–54 km below UB to 40–45 km below WRB.All three crustal layers (upper, middle, and lower) have their maximum depth in the contact zone between UB and the WRB. Below WRB, a lower crust with Vp ~6.7–6.9 km/s is observed. High velocity lower crust was observed below UB (Vp ~7.2 km/s) and possibly below SA (Vp ~7.35 km/s). The modelling was based on ray tracing, using the extrapolation of seismic wave arrival times with the help of travel times predicted from a one-dimensional velocity model. The resulting two-dimensional velocity model partly relies on data from the intersecting DSS profiles and supports previous observations of the lithospheric structure of southeastern Fennoscandia.