Javascript must be enabled to continue!
Stress transfer in the western boundary of Bayan Har Block in Tibet Plateau from the 2008 to 2020 Yutian Earthquake sequence in China
View through CrossRef
Eight M≥7.0 earthquakes have occurred around Bayan Har block since 2000,
resulting huge casualties and countless economic loss. Specifically,
four M≥6.0 earthquakes occurred near the western boundary of Bayan Har
block from 2008 to 2020. Stress interactions among them are
comprehensively investigated by applying ETAS (epidemic-type aftershock
sequence) model and calculating dCFS (Coulomb failure stress change).
The viscoelastic dCFS induced by proceeding Yutian earthquakes on
hypocenters of 2012, 2014 and 2020 Yutian earthquakes are
-1.5004×10
-4
, 3.5820×10
-3
and
1.4770×10
-1
MPa, respectively. The background
probabilities of 2008, 2012, 2014 and 2020 Yutian earthquakes are 0.87,
0.97, 1.5×10
-3
and 8.7×10
-5
,
respectively. Combining those two kinds of evidence, we conclude that
2008 and 2012 Yutian earthquakes are more like background earthquakes
and 2014 and 2020 Yutian earthquakes are triggered by proceeding Yutian
earthquakes.
Title: Stress transfer in the western boundary of Bayan Har Block in Tibet Plateau from the 2008 to 2020 Yutian Earthquake sequence in China
Description:
Eight M≥7.
0 earthquakes have occurred around Bayan Har block since 2000,
resulting huge casualties and countless economic loss.
Specifically,
four M≥6.
0 earthquakes occurred near the western boundary of Bayan Har
block from 2008 to 2020.
Stress interactions among them are
comprehensively investigated by applying ETAS (epidemic-type aftershock
sequence) model and calculating dCFS (Coulomb failure stress change).
The viscoelastic dCFS induced by proceeding Yutian earthquakes on
hypocenters of 2012, 2014 and 2020 Yutian earthquakes are
-1.
5004×10
-4
, 3.
5820×10
-3
and
1.
4770×10
-1
MPa, respectively.
The background
probabilities of 2008, 2012, 2014 and 2020 Yutian earthquakes are 0.
87,
0.
97, 1.
5×10
-3
and 8.
7×10
-5
,
respectively.
Combining those two kinds of evidence, we conclude that
2008 and 2012 Yutian earthquakes are more like background earthquakes
and 2014 and 2020 Yutian earthquakes are triggered by proceeding Yutian
earthquakes.
Related Results
Marina miljön i 8+fjordar – nuvarande kunskap om ekosystemet och de mänskliga belastningarna
Marina miljön i 8+fjordar – nuvarande kunskap om ekosystemet och de mänskliga belastningarna
8+fjordar-området är topografiskt väldigt varierande. Vattenutbytet är långsamt och tillförseln av näringsämnen stor. Största delen av näringsämnen stannar kvar i fjordarna. Mest i...
Stress Transfer Along the Western Boundary of the Bayan Har Block on the Tibet Plateau From the 2008 to 2020 Yutian Earthquake Sequence in China
Stress Transfer Along the Western Boundary of the Bayan Har Block on the Tibet Plateau From the 2008 to 2020 Yutian Earthquake Sequence in China
Abstract
Eight Ml ≥ 7.0 earthquakes have occurred around the Bayan Har block, NW Tibet, China, since 2000, resulting in a large number of cas...
Stress transfer along the western boundary of the Bayan Har Block on the Tibet Plateau from the 2008 to 2020 Yutian earthquake sequence in China
Stress transfer along the western boundary of the Bayan Har Block on the Tibet Plateau from the 2008 to 2020 Yutian earthquake sequence in China
Eight Ml≥7.0 earthquakes have occurred around the Bayan Har block, NW
Tibet, China, since 2000, resulting in a large number of casualties and
countless economic loss. Near the west...
Decomposition and Evolution of Intracontinental Strike‐Slip Faults in Eastern Tibetan Plateau
Decomposition and Evolution of Intracontinental Strike‐Slip Faults in Eastern Tibetan Plateau
Abstract:Little attention had been paid to the intracontinental strike‐slip faults of the Tibetan Plateau. Since the discovery of the Longriba fault using re‐measured GPS data in 2...
Normal Faulting Movement During the 2020 Mw 6.4 Yutian Earthquake: A Shallow Rupture in NW Tibet Revealed by Geodetic Measurements
Normal Faulting Movement During the 2020 Mw 6.4 Yutian Earthquake: A Shallow Rupture in NW Tibet Revealed by Geodetic Measurements
Abstract
The ENE striking Longmu Co fault and the North Altyn Tagh left-lateral slip fault have led to the complex regional structure in the northwestern Tibetan Plateau, r...
Sedimentary Evolution of the Qinghai–Tibet Plateau in Cenozoic and its Response to the Uplift of the Plateau
Sedimentary Evolution of the Qinghai–Tibet Plateau in Cenozoic and its Response to the Uplift of the Plateau
Abstract:We have studied the evolution of the tectonic lithofacies paleogeography of Paleocene–Eocene, Oligocene, Miocene, and Pliocene of the Qinghai–Tibet Plateau by compiling da...
The Complex and Well-Developed Morphological and Histological Structures of the Gastrointestinal Tract of the Plateau Zokor Improve Its Digestive Adaptability to High-Fiber Foods
The Complex and Well-Developed Morphological and Histological Structures of the Gastrointestinal Tract of the Plateau Zokor Improve Its Digestive Adaptability to High-Fiber Foods
The morphological and histological traits of the gastrointestinal tract (GIT) enable the animal to perform some specific functions that enhance the species’ adaptability to environ...

