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1-20 OF 55 RESULTS FOR
ChinArray
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Journal Article
Sensor Misorientation of CHINArray‐II in Northeastern Tibetan Plateau from P ‐ and Rayleigh‐Wave Polarization Analysis
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 19 January 2024
Seismological Research Letters (2024) 95 (3): 1663–1674.
.... In this study, we used three distinct P ‐wave and Rayleigh‐wave polarization analysis methods to estimate actual sensor orientation of 660 stations from CHINArray‐II in northeastern margin of Tibetan plateau. We found that ∼42.12%–45.76% of the stations are well oriented with the absolute misorientation angle...
Includes: Supplemental Content
Journal Article
Ambient Noise Level in Eastern North China from ChinArray and Its Response to COVID‐19
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 21 July 2021
Seismological Research Letters (2021) 92 (6): 3586–3601.
... noise level has been observed to be reduced on a worldwide scale. The continuous waveform data at dense broadband seismic stations from ChinArray in eastern North China provides a good opportunity to study the temporal and spatial patterns of the ambient noise level in the region, and to further study...
Includes: Supplemental Content
Journal Article
Measurements of Seismometer Orientation of the First Phase CHINArray and Their Implications on Vector‐Recording‐Based Seismic Studies
Publisher: Seismological Society of America
Published: 06 October 2020
Bulletin of the Seismological Society of America (2021) 111 (1): 36–49.
...Sijia Zeng; Yong Zheng; Fenglin Niu; Sanxi Ai ABSTRACT From 2011 to 2013, the CHINArray project led by the Institute of Geophysics, China Earthquake Administration, made the first phase deployment of 350 broadband seismometers at the southeastern margin of the Tibetan plateau. The three‐component...
Includes: Supplemental Content
Image
Backprojection results from (a) ChinArray and (b) USArray. (c) The combined...
in Resolvability of Multiple Microseismic P ‐Wave Source Regions with Two Large Seismic Arrays in China and the United States
> Seismological Research Letters
Published: 04 January 2024
Figure 5. Backprojection results from (a) ChinArray and (b) USArray. (c) The combined results by summing the backprojections from ChinArray and USArray. (d) The sources region defined with intersect regions of the source determined by the backprojections from ChinArray and USArray. The same time
Image
Location and array configuration of the ChinArray (left) and USArray (right...
in Resolvability of Multiple Microseismic P ‐Wave Source Regions with Two Large Seismic Arrays in China and the United States
> Seismological Research Letters
Published: 04 January 2024
Figure 1. Location and array configuration of the ChinArray (left) and USArray (right). ChinArray has 379 stations, and USArray has 360. The color version of this figure is available only in the electronic edition.
Image
Example for the locations of P ‐wave microseisms from ChinArray (left colu...
in Resolvability of Multiple Microseismic P ‐Wave Source Regions with Two Large Seismic Arrays in China and the United States
> Seismological Research Letters
Published: 04 January 2024
Figure 4. Example for the locations of P ‐wave microseisms from ChinArray (left column) and USArray (right column), respectively. The time center is 02:00:00, 3 February 2014. The length of the time window is 4 hr. The period ranges of 2.5–5, 5–10, and 10–20 s are used. The color version
Image
(a) Map of 438 ChinArray stations (open triangles) in southwest China. The ...
in Interference of Teleseismic Body Waves in Noise Cross‐Correlation Functions in Southwest China
> Seismological Research Letters
Published: 25 July 2018
Figure 1. (a) Map of 438 ChinArray stations (open triangles) in southwest China. The gray lines are 668 noise cross‐correlation function (NCF) paths with distance 550–650 km whose midpoints are close to array center (black star). The 129 stations comprising these paths are shown as solid
Image
Effect of array aperture on the resolution of the P ‐wave microseisms sour...
in Resolvability of Multiple Microseismic P ‐Wave Source Regions with Two Large Seismic Arrays in China and the United States
> Seismological Research Letters
Published: 04 January 2024
Figure 9. Effect of array aperture on the resolution of the P ‐wave microseisms source locations. For each subplot of (a)–(d), the top panel shows the stations selected from the array for testing, and the bottom panel shows the corresponding relocated results. Panel (a) used the whole ChinArray
Journal Article
Resolvability of Multiple Microseismic P ‐Wave Source Regions with Two Large Seismic Arrays in China and the United States
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 04 January 2024
Seismological Research Letters (2024) 95 (3): 1885–1898.
...Figure 5. Backprojection results from (a) ChinArray and (b) USArray. (c) The combined results by summing the backprojections from ChinArray and USArray. (d) The sources region defined with intersect regions of the source determined by the backprojections from ChinArray and USArray. The same time...
Includes: Supplemental Content
Image
(a,b) Theoretical array response function at a period of 6.67 s for individ...
in Resolvability of Multiple Microseismic P ‐Wave Source Regions with Two Large Seismic Arrays in China and the United States
> Seismological Research Letters
Published: 04 January 2024
Figure 3. (a,b) Theoretical array response function at a period of 6.67 s for individual arrays. (c) The combined results by summing the backprojections from ChinArray and USArray. (d) The sources region defined with intersect regions of the source determined by the backprojections from ChinArray
Image
Global detection scope for teleseismic P ‐wave microseisms determined by g...
in Resolvability of Multiple Microseismic P ‐Wave Source Regions with Two Large Seismic Arrays in China and the United States
> Seismological Research Letters
Published: 04 January 2024
Figure 2. Global detection scope for teleseismic P ‐wave microseisms determined by geographical boundaries used for backprojecting data from ChinArray and USArray. The color version of this figure is available only in the electronic edition.
Journal Article
Deep Slip Rates Along the Fault Zones of the 1927 M 8 Gulang Earthquake Estimated from Repeating Microearthquakes
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 14 November 2024
Seismological Research Letters (2024)
... earthquake occurred with repeating earthquake sequences. We used waveform data recorded by three digital seismic networks from 2001 to 2019 and the second phase of the CHINArray deployment between February 2013 to March 2016. Because of the sparsity of the network in the study area, we employed an empirical...
Includes: Supplemental Content
Journal Article
Interference of Teleseismic Body Waves in Noise Cross‐Correlation Functions in Southwest China
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 25 July 2018
Seismological Research Letters (2018) 89 (5): 1817–1825.
...Figure 1. (a) Map of 438 ChinArray stations (open triangles) in southwest China. The gray lines are 668 noise cross‐correlation function (NCF) paths with distance 550–650 km whose midpoints are close to array center (black star). The 129 stations comprising these paths are shown as solid...
Journal Article
A New Uniform Moment Tensor Catalog for Yunnan, China, from January 2000 through December 2014
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 05 February 2020
Seismological Research Letters (2020) 91 (2A): 891–900.
... ChinArray deployment, we present 1833 moment tensor solutions for small‐to‐moderate earthquakes that occurred between January 2000 and December 2014. Moment magnitudes in the new catalog vary from M w 2.2 to 6.1, and the catalog is complete above M w ∼ 3.5 – 3.6 . The moment tensors are constrained...
Image
(a) Topographic map showing the Tibetan plateau and its surrounding areas. ...
in Measurements of Seismometer Orientation of the First Phase CHINArray and Their Implications on Vector‐Recording‐Based Seismic Studies
> Bulletin of the Seismological Society of America
Published: 06 October 2020
Figure 1. (a) Topographic map showing the Tibetan plateau and its surrounding areas. Black lines indicate boundaries of plates and tectonic blocks. The rectangle indicates the southeastern margin of the Tibetan plateau where the CHINArray phase 1 deployment is located. The margin also marks
Image
Another example of an enlarged P ‐wave microseism source map in the North ...
in Resolvability of Multiple Microseismic P ‐Wave Source Regions with Two Large Seismic Arrays in China and the United States
> Seismological Research Letters
Published: 04 January 2024
Figure 7. Another example of an enlarged P ‐wave microseism source map in the North Pacific for the time centered at 12:00:00, 4 January 2015. Source locations of P ‐wave microseisms of the beam power from the backprojection results of (a) ChinArray, (b) USArray and the combined results
Image
Source locations and regions of P ‐wave microseisms confined by the contou...
in Resolvability of Multiple Microseismic P ‐Wave Source Regions with Two Large Seismic Arrays in China and the United States
> Seismological Research Letters
Published: 04 January 2024
Figure 6. Source locations and regions of P ‐wave microseisms confined by the contour line of the gradient value of the beam power from the backprojection results of (a) ChinArray, (b) USArray, and the combined results of these two arrays through (c) summing and (d) intersecting. (e) Comparison
Image
Distribution of seismic stations (triangles) and hypocenters of selected ea...
in Fluids Triggered the 2021 M w 6.1 Yangbi Earthquake at an Unmapped Fault: Implications for the Tectonics at the Northern End of the Red River Fault
> Seismological Research Letters
Published: 12 January 2022
Figure 2. Distribution of seismic stations (triangles) and hypocenters of selected earthquakes (circles). The black triangles denote permanent stations, and the magenta triangles denote temporary stations of ChinArray phase I. The magenta star denotes the location of the Yangbi earthquake
Journal Article
Fluids Triggered the 2021 M w 6.1 Yangbi Earthquake at an Unmapped Fault: Implications for the Tectonics at the Northern End of the Red River Fault
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 12 January 2022
Seismological Research Letters (2022) 93 (2A): 666–679.
...Figure 2. Distribution of seismic stations (triangles) and hypocenters of selected earthquakes (circles). The black triangles denote permanent stations, and the magenta triangles denote temporary stations of ChinArray phase I. The magenta star denotes the location of the Yangbi earthquake...
Includes: Supplemental Content
Image
(a) Distribution of stations used in this study; all are within Yunnan Prov...
in A New Uniform Moment Tensor Catalog for Yunnan, China, from January 2000 through December 2014
> Seismological Research Letters
Published: 05 February 2020
Figure 2. (a) Distribution of stations used in this study; all are within Yunnan Province. Black triangles represent the 24 stations active since 2000, while black stars represent the 22 stations active since 2007. Diamonds represent the 240 ChinArray stations active in 2012–2013. (b) Epicenters
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