Precursory stress changes before large earthquakes; on a new physical law for earthquakes. (December 2020)

• Record Type: Journal Article
• Authors: Žalohar, Jure; Vičič, Blaž; Potočnik, Matic; Soklič, Nejc; Komac, Marko; Hölscher, Thomas; Herlec, Uroš; Dolenec, Matej
• Is Part Of: Journal of structural geology. Volume 141(2020)
• Publication Date: 2020-12
• Subjects: Earthquakes -- Tectonic stress -- Tectonic strain -- Shear stress -- Maximum magnitude law -- Earthquake precursors; Geology, Structural -- Periodicals; Géomorphologie structurale -- Périodiques; Geology, Structural; Periodicals; 551.805
• DOI: 10.1016/j.jsg.2020.104208
• Languages: English
• ISSNs: 0191-8141

Abstract

Abstract: In this article, we first review the progress in our understanding of tectonic stresses in the Earth's crust achieved in last three to four decades. We briefly review the literature on roughly four groups of studies; (1) World's Stress Map project (WSM), (2) fault-slip data and paleostress analyses, (3) Coulomb stress transfer, and (4) theories of the generalized continua with emphasis on the Cosserat continuum. Based on these studies, we develop a new numerical algorithm to calculate tectonic strain rate, tectonic stress, and normalized tectonic shear stress fields from the earthquake focal mechanisms. We show that this field changes over time, and is therefore far from being constant. Further on, we focus our efforts on the analysis of the relationship between the magnitudes of the earthquakes and the normalized tectonic shear stress. We discover a new and previously unknown physical law, which we call the maximum magnitude law (MM-law). We discuss further the origin and physical background of this law and its importance in earthquake studies. Highlights: We develop new method to calculate the tectonic shear stress in the Earth's crust. We analyze the relation between the shear stress and magnitudes of earthquakes. We discover a new physical law for earthquakes that defines the maximum magnitude. We analyze the shear stress field before the large M7.5+ earthquakes. We discover significant precursory shear stress increase before the large M7.9+ earthquakes.