2002Inland EarthquakeRequires access

PRELIMINARY STUDY ON SEISMOGENIC TECTONIC BACKGROUND OF KUNLUN M_S=8.1 EARTHQUAKE ON NOV.14, 2001 ON THE JUNCTURE OF XINJIANG AND QINGHAI, CHINA

Ruibin Zhao

Open publisher page 3 citations

Abstract

On Nov.14, 2001, a M\-S=8.1 earthquake occurred on the western segment of East Kunlun fault, the boundary of Xinjiang and Qinhai. The East Kunlun fault is a huge boundary fault between two blocks. It has the sinistral shearing due to the eastward escaping of the northeastern part of the Tibetan Plateau, which is a famous strong earthquake belt in north Tibetan Plateau. The M\-S=8.1 quake was centered in the conjunction of the NWW-trending East Kunlun fault and a NEE-trending secondary fault. The rupture is mono-propagating from the west to the east.

About this research paper

What this paper is about

On Nov.14, 2001, a M\-S=8.1 earthquake occurred on the western segment of East Kunlun fault, the boundary of Xinjiang and Qinhai. The East Kunlun fault is a huge boundary fault between two blocks. It has the sinistral shearing due to the eastward escaping of the northeastern part of the Tibetan Plateau, which is a famous strong earthquake belt in north Tibetan Plateau. The M\-S=8.1 quake was centered in the conjunction of the NWW-trending East Kunlun fault and a NEE-trending secondary fault. The rupture is mono-propagating from the west to the east.

Why it matters

OpenAlex reports 3 citations for this work. Citation counts describe recorded attention and do not establish research quality.

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

On Nov.14, 2001, a M\-S=8.1 earthquake occurred on the western segment of East Kunlun fault, the boundary of Xinjiang and Qinhai. The East Kunlun fault is a huge boundary fault between two blocks. It has the sinistral shearing due to the eastward escaping of the northeastern part of the Tibetan Plateau, which is a famous strong earthquake belt in north Tibetan Plateau. The M\-S=8.1 quake was centered in the conjunction of the NWW-trending East Kunlun fault and a NEE-trending secondary fault. The rupture is mono-propagating from the west to the east.

Key concepts: Geology, Seismology, Sinistral and dextral, Plateau (mathematics), Tectonics, Quake (natural phenomenon), Intraplate earthquake, Fault (geology)

Related papers

Back to paper searchBrowse research topicsOriginal source
PRELIMINARY STUDY ON SEISMOGENIC TECTONIC BACKGROUND OF KUNLUN M_S=8.1 EARTHQUAKE ON NOV.14, 2001 ON THE JUNCTURE OF XINJIANG AND QINGHAI, CHINA — Research Paper | ScholarLens