Crustal structure and magmatic evolution in the Pearl River Delta of the Cathaysia Block: New constraints from receiver function modeling

We used teleseismic data recorded at 17 permanent seismic stations operated by the China Earthquake Administration. Teleseismic waveforms from events with magnitudes ≥ 6.0 and with epicentral distances of 30° to 90° were chosen to estimate receiver functions beneath the stations. The earthquakes mai...

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Bibliographic Details
Main Author: Huang, Haibo
Other Authors: Haibo Huang
Format: Dataset
Language:unknown
Published: Mendeley 2019
Subjects:
geo
Online Access:https://doi.org/10.17632/T8896TJJGP
https://doi.org/10.17632/t8896tjjgp.1
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spelling fttriple:oai:gotriple.eu:50|dedup_wf_001::0b462e36d036d7618a03c70c87401782 2023-05-15T13:14:42+02:00 Crustal structure and magmatic evolution in the Pearl River Delta of the Cathaysia Block: New constraints from receiver function modeling Huang, Haibo Haibo Huang 2019-08-07 https://doi.org/10.17632/T8896TJJGP https://doi.org/10.17632/t8896tjjgp.1 undefined unknown Mendeley http://dx.doi.org/10.17632/T8896TJJGP http://dx.doi.org/10.17632/t8896tjjgp.1 https://dx.doi.org/10.17632/t8896tjjgp.1 https://dx.doi.org/10.17632/t8896tjjgp lic_creative-commons doi:10.17632/t8896tjjgp 10.17632/t8896tjjgp.1 oai:easy.dans.knaw.nl:easy-dataset:131506 oai:oai.datacite.org:21937236 oai:services.nod.dans.knaw.nl:Products/dans:oai:easy.dans.knaw.nl:easy-dataset:131506 10.17632/t8896tjjgp doi:10.17632/t8896tjjgp.1 oai:oai.datacite.org:21937235 10|re3data_____::db814dc656a911b556dba42a331cebe9 10|openaire____::9e3be59865b2c1c335d32dae2fe7b254 10|re3data_____::84e123776089ce3c7a33db98d9cd15a8 10|eurocrisdris::fe4903425d9040f680d8610d9079ea14 Database Interdisciplinary sciences geo manag Dataset https://vocabularies.coar-repositories.org/resource_types/c_ddb1/ 2019 fttriple https://doi.org/10.17632/T8896TJJGP https://doi.org/10.17632/t8896tjjgp.1 https://doi.org/10.17632/t8896tjjgp 2023-01-22T17:41:32Z We used teleseismic data recorded at 17 permanent seismic stations operated by the China Earthquake Administration. Teleseismic waveforms from events with magnitudes ≥ 6.0 and with epicentral distances of 30° to 90° were chosen to estimate receiver functions beneath the stations. The earthquakes mainly occurred along the Kurile and Aleutian island arcs, north of Australia, Indonesia and the Tibet continental collision zone. The seismograms were manually checked to extract the data with high signal-to-noise ratio. The traces were windowed to include 30 s before and 100 s after the direct P-wave arrivals, and then horizontal components were rotated into radial and transverse components. We computed receiver functions using the source equalization procedure with a water-level parameter of 0.001 and a Gaussian width of 2.5. The final receiver functions were further checked based on noise level of the signals before the direct P-wave arrivals as well as the shape of the following converted phases. Dataset Aleutian Island Unknown
institution Open Polar
collection Unknown
op_collection_id fttriple
language unknown
topic Database
Interdisciplinary sciences
geo
manag
spellingShingle Database
Interdisciplinary sciences
geo
manag
Huang, Haibo
Crustal structure and magmatic evolution in the Pearl River Delta of the Cathaysia Block: New constraints from receiver function modeling
topic_facet Database
Interdisciplinary sciences
geo
manag
description We used teleseismic data recorded at 17 permanent seismic stations operated by the China Earthquake Administration. Teleseismic waveforms from events with magnitudes ≥ 6.0 and with epicentral distances of 30° to 90° were chosen to estimate receiver functions beneath the stations. The earthquakes mainly occurred along the Kurile and Aleutian island arcs, north of Australia, Indonesia and the Tibet continental collision zone. The seismograms were manually checked to extract the data with high signal-to-noise ratio. The traces were windowed to include 30 s before and 100 s after the direct P-wave arrivals, and then horizontal components were rotated into radial and transverse components. We computed receiver functions using the source equalization procedure with a water-level parameter of 0.001 and a Gaussian width of 2.5. The final receiver functions were further checked based on noise level of the signals before the direct P-wave arrivals as well as the shape of the following converted phases.
author2 Haibo Huang
format Dataset
author Huang, Haibo
author_facet Huang, Haibo
author_sort Huang, Haibo
title Crustal structure and magmatic evolution in the Pearl River Delta of the Cathaysia Block: New constraints from receiver function modeling
title_short Crustal structure and magmatic evolution in the Pearl River Delta of the Cathaysia Block: New constraints from receiver function modeling
title_full Crustal structure and magmatic evolution in the Pearl River Delta of the Cathaysia Block: New constraints from receiver function modeling
title_fullStr Crustal structure and magmatic evolution in the Pearl River Delta of the Cathaysia Block: New constraints from receiver function modeling
title_full_unstemmed Crustal structure and magmatic evolution in the Pearl River Delta of the Cathaysia Block: New constraints from receiver function modeling
title_sort crustal structure and magmatic evolution in the pearl river delta of the cathaysia block: new constraints from receiver function modeling
publisher Mendeley
publishDate 2019
url https://doi.org/10.17632/T8896TJJGP
https://doi.org/10.17632/t8896tjjgp.1
genre Aleutian Island
genre_facet Aleutian Island
op_source doi:10.17632/t8896tjjgp
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oai:easy.dans.knaw.nl:easy-dataset:131506
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oai:services.nod.dans.knaw.nl:Products/dans:oai:easy.dans.knaw.nl:easy-dataset:131506
10.17632/t8896tjjgp
doi:10.17632/t8896tjjgp.1
oai:oai.datacite.org:21937235
10|re3data_____::db814dc656a911b556dba42a331cebe9
10|openaire____::9e3be59865b2c1c335d32dae2fe7b254
10|re3data_____::84e123776089ce3c7a33db98d9cd15a8
10|eurocrisdris::fe4903425d9040f680d8610d9079ea14
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