Abstrakt
In this work, we perform a seismological investigation in the central Brazil region for focal mechanisms and stress. This large area (910.000 km(2)) is surrounded by several geological provinces: Eastem Amazon craton; southwestern Parnaiba basin; western Sao Francisco craton; northern Parana basin and almost the whole Tocantins province.
The area is crossed, in an SW-NE direction, by the continental-scale discontinuity - Transbrasiliano lineament (LTB). In the Brazilian seismic catalog (1720-2019), it is possible to distinguish a seismic belt following the LTB lineament and some dispersed events in the northern, western and eastern areas.
The study area is characterized mainly by low magnitude events (M 4 occurred, and among them just one with magnitude 5. Based on quality criteria a set of 118 events from 338 present in the catalog were selected for a thorough analysis.
This work was divided in three parts: (i) Events relocation with the iLoc code and Regional Seismic Travel Time (RSTT) velocity model; (ii) Focal mechanisms determination of 10 events using waveform envelopes inversion and polarities, and; (iii) Inversion of focal mechanisms for stress field. The study shows that the seismicity of the area is mainly concentrated in two relatively narrow belts and that the major compressional stress axis of the whole zone is well resolved with azimuth about 133 degrees which is compatible with previous studies of stress in central Brazil.