2004Inland EarthquakeRequires access

STUDY OF THE STRAIN ANOMALY ABOUT THE FAR FIELD BEFORE THE EARTHQUAKE WITH M_S8.1 IN WEST KUNLUN MOUNTAIN

Tao Tian

Open publisher page 0 citations

Abstract

According to the continuous observation data of the borehole stress-strain of 6 stations, we studied the variance of the region stress field. The result showed that the stress field around the Qinghai-Xizang plateau appeared some marked variance in Oct. 2000. By comparing with the time-space distribution of seismic activities before the earthquake with M_S8.1 in the west Kunlun mountain, we discovered that it is the result of stress concentration release about the Xinghai earthquake swarm in Sept. 2000 and the Tanggula swarm from Oct. to Nov. of 2000 in the seismogenic process of the earthquake with M_S8.1 of the west Kunlun mountain.

About this research paper

What this paper is about

According to the continuous observation data of the borehole stress-strain of 6 stations, we studied the variance of the region stress field. The result showed that the stress field around the Qinghai-Xizang plateau appeared some marked variance in Oct. 2000. By comparing with the time-space distribution of seismic activities before the earthquake with M_S8.1 in the west Kunlun mountain, we discovered that it is the result of stress concentration release about the Xinghai earthquake swarm in Sept. 2000 and the Tanggula swarm from Oct. to Nov. of 2000 in the seismogenic process of the earthquake with M_S8.1 of the west Kunlun mountain.

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

According to the continuous observation data of the borehole stress-strain of 6 stations, we studied the variance of the region stress field. The result showed that the stress field around the Qinghai-Xizang plateau appeared some marked variance in Oct. 2000. By comparing with the time-space distribution of seismic activities before the earthquake with M_S8.1 in the west Kunlun mountain, we discovered that it is the result of stress concentration release about the Xinghai earthquake swarm in Sept. 2000 and the Tanggula swarm from Oct. to Nov. of 2000 in the seismogenic process of the earthquake with M_S8.1 of the west Kunlun mountain.

Key concepts: Geology, Earthquake swarm, Plateau (mathematics), Seismology, Stress field, Anomaly (physics), Borehole, Intraplate earthquake

Related papers

Back to paper searchBrowse research topicsOriginal source
STUDY OF THE STRAIN ANOMALY ABOUT THE FAR FIELD BEFORE THE EARTHQUAKE WITH M_S8.1 IN WEST KUNLUN MOUNTAIN — Research Paper | ScholarLens