Seismic data acquisition including survey design and factors affecting seismic acquisition

Geophysicists collect seismic data in the same way as earthquake seismologists. Elastic waves propagate through the Earth as a result of earthquakes. The ground motions caused by elastic wave propagation are then recorded by seismologists using a seismograph. A controlled seismic source of energy, b...

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Main Authors: Md Arshad, A.R., Abdul Latiff, A.H., Bashir, Y.
Format: Book
Published: Elsevier 2022
Online Access:http://scholars.utp.edu.my/id/eprint/34100/
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85138355476&doi=10.1016%2fB978-0-323-91946-3.00006-7&partnerID=40&md5=5b751d287409c8429a07b45f464f430e
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Institution: Universiti Teknologi Petronas
id oai:scholars.utp.edu.my:34100
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spelling oai:scholars.utp.edu.my:341002023-01-03T07:22:55Z http://scholars.utp.edu.my/id/eprint/34100/ Seismic data acquisition including survey design and factors affecting seismic acquisition Md Arshad, A.R. Abdul Latiff, A.H. Bashir, Y. Geophysicists collect seismic data in the same way as earthquake seismologists. Elastic waves propagate through the Earth as a result of earthquakes. The ground motions caused by elastic wave propagation are then recorded by seismologists using a seismograph. A controlled seismic source of energy, but one that is much lower than an earthquake, is used in seismic exploration to generate elastic waves that propagate through the subsurface. Multiple receivers at the surface detect and record reflected seismic energy. © 2022 Elsevier Inc. All rights reserved. Elsevier 2022 Book NonPeerReviewed Md Arshad, A.R. and Abdul Latiff, A.H. and Bashir, Y. (2022) Seismic data acquisition including survey design and factors affecting seismic acquisition. Elsevier, pp. 1-17. ISBN 9780323919463; 9780323918879 https://www.scopus.com/inward/record.uri?eid=2-s2.0-85138355476&doi=10.1016%2fB978-0-323-91946-3.00006-7&partnerID=40&md5=5b751d287409c8429a07b45f464f430e 10.1016/B978-0-323-91946-3.00006-7 10.1016/B978-0-323-91946-3.00006-7 10.1016/B978-0-323-91946-3.00006-7
institution Universiti Teknologi Petronas
building UTP Resource Centre
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknologi Petronas
content_source UTP Institutional Repository
url_provider http://eprints.utp.edu.my/
description Geophysicists collect seismic data in the same way as earthquake seismologists. Elastic waves propagate through the Earth as a result of earthquakes. The ground motions caused by elastic wave propagation are then recorded by seismologists using a seismograph. A controlled seismic source of energy, but one that is much lower than an earthquake, is used in seismic exploration to generate elastic waves that propagate through the subsurface. Multiple receivers at the surface detect and record reflected seismic energy. © 2022 Elsevier Inc. All rights reserved.
format Book
author Md Arshad, A.R.
Abdul Latiff, A.H.
Bashir, Y.
spellingShingle Md Arshad, A.R.
Abdul Latiff, A.H.
Bashir, Y.
Seismic data acquisition including survey design and factors affecting seismic acquisition
author_facet Md Arshad, A.R.
Abdul Latiff, A.H.
Bashir, Y.
author_sort Md Arshad, A.R.
title Seismic data acquisition including survey design and factors affecting seismic acquisition
title_short Seismic data acquisition including survey design and factors affecting seismic acquisition
title_full Seismic data acquisition including survey design and factors affecting seismic acquisition
title_fullStr Seismic data acquisition including survey design and factors affecting seismic acquisition
title_full_unstemmed Seismic data acquisition including survey design and factors affecting seismic acquisition
title_sort seismic data acquisition including survey design and factors affecting seismic acquisition
publisher Elsevier
publishDate 2022
url http://scholars.utp.edu.my/id/eprint/34100/
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85138355476&doi=10.1016%2fB978-0-323-91946-3.00006-7&partnerID=40&md5=5b751d287409c8429a07b45f464f430e
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