Abstract:A New Paradigm (data driven and not like the currently model driven) is needed for Reliable Seismic Hazard Assessment RSHA. Neo-Deterministic Seismic Hazard Assessment (NDSHA) integrates earthquake geology, earthquake science, and particularly earthquake physics to finally achieve a New (and needed) Paradigm for Reliable Seismic Hazard Assessment RSHA.Although observations from many recent destructive earthquakes have all confirmed the validity of NDSHA’s approach and application to earthquake hazard forecasti… Show more
“…NDSHA has been described in numerous previous studies (NDSHA, Panza et al, 2001;2012;Panza and Bela, 2020;Bela and Panza, 2021;Panza et al, 2021), which detail the theoretical framework and computational workflow. Here, we summarize the main steps and describe the specific input data used in this study.…”
Section: Methodology and Data Usedmentioning
confidence: 99%
“…Left: tectonic setting of Kosovo (red square), after Burchfiel et al, (2008); right: seismicity of the study area from the SHEEC catalogue (M W ≥5). For color code, please refer to the digital version of the paper In this study, we present seismic hazard maps generated using the well-established Neo-Deterministic Seismic Hazard Assessment (NDSHA) methodology (Panza et al, 2001;2012;Panza and Bela, 2020;Bela and Panza, 2021;Panza et al, 2021).…”
Kosovo is one of the most seismically active regions in Europe, lying within the Alpine-Mediterranean tectonic belt. Historical records for the region show several catastrophic earthquakes with epicentral intensity IX (MCS). However, due to Kosovo’s high population density, high prevalence of traditional construction, and insufficient enforcement of building codes, Kosovo is vulnerable to earthquake damage. In this study, we present earthquake hazard maps for bedrock conditions in Kosovo based on the well-known Neo-deterministic Seismic Hazard Assessment (NDSHA) method. NDSHA relies upon the fundamental physics of wave generation and propagation in complex geologic structures to generate realistic time series, used as input for the computation of several ground motion parameters, integrating the available knowledge of seismic history, seismogenic zones and morphostructural nodes. In accordance with continuum mechanics, the tensor nature of earthquake ground motion is preserved, producing realistic signals using structural models obtained by tomographic inversion and earthquake source information readily available in literature. Our maps are generally consistent with the observed intensity IX (MCS) and suggest that, in some instances, intensity X could be reached.
“…NDSHA has been described in numerous previous studies (NDSHA, Panza et al, 2001;2012;Panza and Bela, 2020;Bela and Panza, 2021;Panza et al, 2021), which detail the theoretical framework and computational workflow. Here, we summarize the main steps and describe the specific input data used in this study.…”
Section: Methodology and Data Usedmentioning
confidence: 99%
“…Left: tectonic setting of Kosovo (red square), after Burchfiel et al, (2008); right: seismicity of the study area from the SHEEC catalogue (M W ≥5). For color code, please refer to the digital version of the paper In this study, we present seismic hazard maps generated using the well-established Neo-Deterministic Seismic Hazard Assessment (NDSHA) methodology (Panza et al, 2001;2012;Panza and Bela, 2020;Bela and Panza, 2021;Panza et al, 2021).…”
Kosovo is one of the most seismically active regions in Europe, lying within the Alpine-Mediterranean tectonic belt. Historical records for the region show several catastrophic earthquakes with epicentral intensity IX (MCS). However, due to Kosovo’s high population density, high prevalence of traditional construction, and insufficient enforcement of building codes, Kosovo is vulnerable to earthquake damage. In this study, we present earthquake hazard maps for bedrock conditions in Kosovo based on the well-known Neo-deterministic Seismic Hazard Assessment (NDSHA) method. NDSHA relies upon the fundamental physics of wave generation and propagation in complex geologic structures to generate realistic time series, used as input for the computation of several ground motion parameters, integrating the available knowledge of seismic history, seismogenic zones and morphostructural nodes. In accordance with continuum mechanics, the tensor nature of earthquake ground motion is preserved, producing realistic signals using structural models obtained by tomographic inversion and earthquake source information readily available in literature. Our maps are generally consistent with the observed intensity IX (MCS) and suggest that, in some instances, intensity X could be reached.
“…Another edge detection filter based on the ratio of the derivatives of the THG, was proposed by for improving the resolution of results, called the logistic function of the total horizontal gradient, which is given by [53]: (4) where and α is a constant that is decided by the researcher. This constant controls the effectiveness of the method.…”
Section: Methodsmentioning
confidence: 99%
“…Geophysical methods have been used for many years in the determination of nature and processes of the Earth [1][2][3][4][5][6][7], and gravity method is one of the oldest methods used to solve this problem [8,9]. Despite the development of an increasing number of additional exploration techniques, some of which can determine geological structures with higher resolution, the gravity method has continued to be an important and sometimes crucial constraint in a wide variety of terrestrial investigations [8][9][10].…”
An important feature in the interpretation of gravity data is the determination of the edges of the density structures. There are several different enhancement techniques used to achieve the edge locations. In this study, we aim to estimate the effectiveness of some edge enhancement techniques such as the total horizontal gradient, analytic signal, theta map, and logistic function of the total horizontal gradient in terms of their accuracy on detection of subsurface structures from gravity data. These methods were tested on synthetic gravity data with and without noise. Findings show that the logistic function of the total horizontal gradient performs better than other methods under almost all cases. Additionally, the methods are also applied to real gravity data from the Phu Khanh basin as a practical example. The results determined by the LTHG technique reveals the presence of many structures with E-W, NE-SW, NNW-SSE, ENE-WSW, and NNE-SSW trends in the basin.
“…Among the consequences of the widespread idea, albeit unsophisticated, of elastic stress accumulation as the driver of seismic processes are the concept of "seismic cycle" [238,239], "typical earthquake" [240,241] and the seismic gap hypothesis [242,243]. For an alternative critical evaluation of these concepts, see [244]. The first one is an appealing framework concerning temporal distribution of seismicity within sufficiently localized bounded regions in which earthquakes are expected to occur after a period of stress increase due to tectonic forces, once the stress drop has happened, weakening processes are also responsible of a post-seismic phase in which minor events, i.e., aftershocks, are recorded before reaching a new state of mechanical stability.…”
Section: The Effect Of Relative Plate Motionsmentioning
The processes occurring on the Earth are controlled by several gradients. The surface of the Planet is featured by complex geological patterns produced by both endogenous and exogenous phenomena. The lack of direct investigations still makes Earth interior poorly understood and prevents complete clarification of the mechanisms ruling geodynamics and tectonics. Nowadays, slab-pull is considered the force with the greatest impact on plate motions, but also ridge-push, trench suction and physico-chemical heterogeneities are thought to play an important role. However, several counterarguments suggest that these mechanisms are insufficient to explain plate tectonics. While large part of the scientific community agreed that either bottom-up or top-down driven mantle convection is the cause of lithospheric displacements, geodetic observations and geodynamic models also support an astronomical contribution to plate motions. Moreover, several evidences indicate that tectonic plates follow a mainstream and how the lithosphere has a roughly westerly drift with respect to the asthenospheric mantle. An even more wide-open debate rises for the occurrence of earthquakes, which should be framed within the different tectonic setting, which affects the spatial and temporal properties of seismicity. In extensional regions, the dominant source of energy is given by gravitational potential, whereas in strike-slip faults and thrusts, earthquakes mainly dissipate elastic potential energy indeed. In the present article, a review is given of the most significant results of the last years in the field of geodynamics and earthquake geology following the common thread of gradients, which ultimately shape our planet.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.