2001•Unpublished venueRequires access

Characteristic analysis and precursory anomaly in weak seismic region

Wu Fu

Open publisher page 0 citations

Abstract

Based on the data of precursory anomaly observed in Shaanxi Precursory Network, we analyzed the characteristics of precursory anomaly in the regions where there are no or few earthquakes. The ratio of precursory anomaly is between 11% to 20% for different precursory means and the comprehensive ratio of anomaly is 15% in Shaanxi Precursory Network. There is no earthquake with M S ≥5.0 and usually only two to three earthquakes with M S ≥3.0 occurred every year and the average magnitude of maximum earthquakes for every year is M L =3.6. The curve variation between the anomaly ratio, seismic frequency and seismic intensity in Shaanxi region is not synchronal. So, it is concluded that the precursory anomaly is not the earthquake precursor, and it may be the interference unknown or the result of aseismic slipping in crust.

About this research paper

What this paper is about

Based on the data of precursory anomaly observed in Shaanxi Precursory Network, we analyzed the characteristics of precursory anomaly in the regions where there are no or few earthquakes. The ratio of precursory anomaly is between 11% to 20% for different precursory means and the comprehensive ratio of anomaly is 15% in Shaanxi Precursory Network. There is no earthquake with M S ≥5.0 and usually only two to three earthquakes with M S ≥3.0 occurred every year and the average magnitude of maximum earthquakes for every year is M L =3.6. The curve variation between the anomaly ratio, seismic frequency and seismic intensity in Shaanxi region is not synchronal. So, it is concluded that the precursory anomaly is not the earthquake precursor, and it may be the interference unknown or the result of aseismic slipping in crust.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Based on the data of precursory anomaly observed in Shaanxi Precursory Network, we analyzed the characteristics of precursory anomaly in the regions where there are no or few earthquakes. The ratio of precursory anomaly is between 11% to 20% for different precursory means and the comprehensive ratio of anomaly is 15% in Shaanxi Precursory Network. There is no earthquake with M S ≥5.0 and usually only two to three earthquakes with M S ≥3.0 occurred every year and the average magnitude of maximum earthquakes for every year is M L =3.6. The curve variation between the anomaly ratio, seismic frequency and seismic intensity in Shaanxi region is not synchronal. So, it is concluded that the precursory anomaly is not the earthquake precursor, and it may be the interference unknown or the result of aseismic slipping in crust.

Key concepts: Anomaly (physics), Seismology, Geology, Slipping, Magnitude (astronomy), Crust, Geophysics, Physics

Related papers

Back to paper searchBrowse research topicsOriginal source
Characteristic analysis and precursory anomaly in weak seismic region — Research Paper | ScholarLens