Javascript must be enabled to continue!
Space-Time Anomaly Characteristics of Strain Field before the Ms≥7.0 Earthquakes, In Mainland China
View through CrossRef
Abstract
Seismologists focus on analyzing and capturing medium and short-term impending anomalies of medium and small earthquakes before large earthquakes. The natural orthogonal expansion method can effectively extract small and medium seismicity anomalies in the epicentral region before large earthquakes, which can improve the prediction of large earthquakes. In this study, the strain range of small earthquakes that occurred in the Chinese mainland before 1980, specifically ten Ms ≥ 7.0 earthquakes, were calculated, and the temporal and spatial anomalies of the strain fields before the large earthquakes were extracted. The active faults in each large earthquake area were analyzed to identify the dangerous areas (Epicenter of earthquake) of the large earthquake. In addition, compared with the seismic energy field method, the natural orthogonal expansion method effectively captured the short-term and impending anomalies in the seismic strain field before large earthquakes. The results of this study can have a significant impact on the analysis of anomalies by strain field, and make an outstanding contribution to the study of large earthquake prediction.
Title: Space-Time Anomaly Characteristics of Strain Field before the Ms≥7.0 Earthquakes, In Mainland China
Description:
Abstract
Seismologists focus on analyzing and capturing medium and short-term impending anomalies of medium and small earthquakes before large earthquakes.
The natural orthogonal expansion method can effectively extract small and medium seismicity anomalies in the epicentral region before large earthquakes, which can improve the prediction of large earthquakes.
In this study, the strain range of small earthquakes that occurred in the Chinese mainland before 1980, specifically ten Ms ≥ 7.
0 earthquakes, were calculated, and the temporal and spatial anomalies of the strain fields before the large earthquakes were extracted.
The active faults in each large earthquake area were analyzed to identify the dangerous areas (Epicenter of earthquake) of the large earthquake.
In addition, compared with the seismic energy field method, the natural orthogonal expansion method effectively captured the short-term and impending anomalies in the seismic strain field before large earthquakes.
The results of this study can have a significant impact on the analysis of anomalies by strain field, and make an outstanding contribution to the study of large earthquake prediction.
Related Results
Summaries, Analysis and Simulations of Recent COVID-19 Epidemic in Mainland China During December 31 2021-December 6 2022
Summaries, Analysis and Simulations of Recent COVID-19 Epidemic in Mainland China During December 31 2021-December 6 2022
AbstractBackgroundThe recent COVID-19 epidemic in mainland China is an important issue for studying the prevention and disease control measures and the spread of the COVID-19 epide...
Seditious Spaces
Seditious Spaces
The title ‘Seditious Spaces’ is derived from one aspect of Britain’s colonial legacy in Malaysia (formerly Malaya): the Sedition Act 1948. While colonial rule may seem like it was ...
Water relations of an insular pit viper
Water relations of an insular pit viper
Colonization of novel habitats often requires plasticity or adaptation to local conditions. There is a critical need to maintain hydration in terrestrial environments having limite...
Financial Strain and Health
Financial Strain and Health
One of the most fundamental results in health economics is that a greater socio-economic status is associated with better health outcomes. However, the experience of financial pres...
A simple discrete element model for large multiplet earthquakes
A simple discrete element model for large multiplet earthquakes
Adjacent segments of the plate boundary may fail separately as earthquakes that occur very close in time. When the time between events is a small fraction of the recurrence interva...
Testing the Strain-rate Hypothesis for Deep Slab Seismicity
Testing the Strain-rate Hypothesis for Deep Slab Seismicity
<p>The occurrence of deep earthquakes within subducting lithosphere (slabs) remains enigmatic because these earthquakes have many similarities to shallow earthquakes,...
Temporal Distribution Model and Occurrence Probability of M≥6.5 Earthquakes in North China Seismic Zone
Temporal Distribution Model and Occurrence Probability of M≥6.5 Earthquakes in North China Seismic Zone
Abstract
The temporal distribution of earthquakes provides important basis for earthquake prediction and seismic hazard analysis. The relatively limited records of strong e...
GLOBAL EARTHQUAKES
GLOBAL EARTHQUAKES
The information on the Earth seismicity in 2013 at the level of strong earthquakes with M≥6 is provided according to the Seismological Bulletin of the Geophysical Survey of RAS (GS...

