Plate boundary forces are not enough: Second‐ and third‐order stress patterns highlighted in the World Stress Map database

TLDR: The World Stress Map Project (WSMP) database as mentioned in this paper provides a global database of contemporary tectonic stress information of the Earth's crust, and the 2005 release of the WSMP database provides, for some areas, high data density that enables us to investigate third-order (local) stress field variations and forces controlling them such as active faults, local inclusions, detachment horizons, and density contrasts.

Abstract: [1] The World Stress Map Project compiles a global database of contemporary tectonic stress information of the Earth's crust. Early releases of the World Stress Map Project demonstrated the existence of first-order (plate-scale) stress fields controlled by plate boundary forces and second-order (regional) stress fields controlled by major intraplate stress sources such as mountain belts and zones of widespread glacial rebound. The 2005 release of the World Stress Map Project database provides, for some areas, high data density that enables us to investigate third-order (local) stress field variations, and the forces controlling them such as active faults, local inclusions, detachment horizons, and density contrasts. These forces act as major controls on the stress field orientations when the magnitudes of the horizontal stresses are close to isotropic. We present and discuss examples for Venezuela, Australia, Romania, Brunei, western Europe, and southern Italy where a substantial increase of data records demonstrates some of the additional factors controlling regional and local stress patterns.