scholarly journals Studying the seismogenic coupling zone with a passive seismic array

Eos ◽  
2005 ◽  
Vol 86 (32) ◽  
pp. 293 ◽  
Author(s):  
A. Rietbrock ◽  
C. Haberland ◽  
K. Bataille ◽  
T. Dahm ◽  
O. Oncken
Keyword(s):  
Seismic Array ◽  
Passive Seismic ◽  
Coupling Zone

scholarly journals Joint imaging by teleseismic converted and multiple waves and its application in the INDEPTH-III passive seismic array

2005 ◽  
Vol 32 (21) ◽  
Author(s):  
Xiaobo Tian ◽  
Qingju Wu ◽  
Zhongjie Zhang ◽  
Jiwen Teng ◽  
Rongsheng Zeng
Keyword(s):  
Seismic Array ◽  
Passive Seismic

Preliminary results from a passive seismic array over the Chicxulub impact structure in Mexico

1998 ◽  
Vol 140 (1) ◽  
pp. 177-193 ◽  
Author(s):  
P. K. H. Maguire ◽  
G. D. Mackenzie ◽  
P. Denton ◽  
A. Trejo ◽  
R. Kind ◽  
...  
Keyword(s):  
Seismic Array ◽  
Impact Structure ◽  
Preliminary Results ◽  
Passive Seismic ◽  
Chicxulub Impact

scholarly journals Geological Survey of South Australia: The AusArray SA passive seismic array and new MT data

Preview ◽  
2021 ◽  
Vol 2021 (212) ◽  
pp. 31-32
Author(s):  
John Paul O’Donnell ◽  
Kate Robertson
Keyword(s):  
South Australia ◽  
Seismic Array ◽  
Geological Survey ◽  
Passive Seismic

scholarly journals Passive seismic experiment ‘AniMaLS’ in the Polish Sudetes (NE Variscides)

2021 ◽  
Author(s):  
Monika Bociarska ◽  
Julia Rewers ◽  
Dariusz Wójcik ◽  
Weronika Materkowska ◽  
Piotr Środa ◽  
...  
Keyword(s):  
Seismic Anisotropy ◽  
Geological Structure ◽  
Seismic Array ◽  
Data Quality Control ◽  
Data Set ◽  
Near Surface ◽  
Correct Orientation ◽  
Seismic Experiment ◽  
Passive Seismic ◽  
Set Up

Abstract. The paper presents information about the seismic experiment AniMaLS which aims to provide a new insight into the crustal and upper mantle structure beneath the Polish Sudetes (NE margin of the Variscan orogen). The seismic array composed of 23 temporary broadband stations was operating continuously for ~2 years (October 2017 and October 2019). The dataset was complemented by records from 8 permanent stations located in the study area and in the vicinity. The stations were deployed with inter-station spacing of approximately 25–30 km. As a result, good quality recordings of local, regional and teleseismic events were obtained. We describe the aims and motivation of the project, the stations deployment procedure, as well as the characteristics of the temporary seismic array and of the permanent stations. Furthermore, this paper includes a description of important issues like: data transmission set-up, status monitoring systems, data quality control, near-surface geological structure beneath stations and related site effects etc. Special attention was paid to verification of correct orientation of the sensors. The obtained data set will be modelled using several seismic interpretation methods, including analysis of seismic anisotropy parameters, with the objective of extending knowledge about the lithospheric and sub-lithospheric structure and the tectonic evolution of the study area.

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