MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK
The theoretical behaviour of guided waves in cross-hole seismic surveys is examined with dispersion curves and synthetic seismograms. The modelling suggests, and field observations confirm, that the dominant energy in many cross-hole seismic surveys propagates as guided waves, as well as body waves,...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
LOU, MIN [verfasserIn] CRAMPIN, STUART [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|
| Erschienen: |
Oxford, UK: Blackwell Publishing Ltd ; 1993 |
|---|
| Umfang: |
Online-Ressource |
|---|
| Reproduktion: |
2006 ; Blackwell Publishing Journal Backfiles 1879-2005 |
|---|---|
| Übergeordnetes Werk: |
In: Geophysical prospecting - Oxford [u.a.] : Wiley-Blackwell, 1953, 41(1993), 3, Seite 0 |
| Übergeordnetes Werk: |
volume:41 ; year:1993 ; number:3 ; pages:0 |
| Links: |
|---|
| DOI / URN: |
10.1111/j.1365-2478.1993.tb00569.x |
|---|
| Katalog-ID: |
NLEJ239605454 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | NLEJ239605454 | ||
| 003 | DE-627 | ||
| 005 | 20210707091538.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 120426s1993 xx |||||o 00| ||und c | ||
| 024 | 7 | |a 10.1111/j.1365-2478.1993.tb00569.x |2 doi | |
| 035 | |a (DE-627)NLEJ239605454 | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 100 | 1 | |a LOU, MIN |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK |
| 264 | 1 | |a Oxford, UK |b Blackwell Publishing Ltd |c 1993 | |
| 300 | |a Online-Ressource | ||
| 336 | |a nicht spezifiziert |b zzz |2 rdacontent | ||
| 337 | |a nicht spezifiziert |b z |2 rdamedia | ||
| 338 | |a nicht spezifiziert |b zu |2 rdacarrier | ||
| 520 | |a The theoretical behaviour of guided waves in cross-hole seismic surveys is examined with dispersion curves and synthetic seismograms. The modelling suggests, and field observations confirm, that the dominant energy in many cross-hole seismic surveys propagates as guided waves, as well as body waves, with the energy tied to an interface, or combination of interfaces, whenever there are interfaces with significant velocity contrasts continuous between the wells. The dispersion and waveforms of such modal solutions carry detailed information about the internal structure, particularly the stress-aligned structure of fluid-filled inclusions in the immediate neighbourhood of the waveguide. Since the information content can be controlled to some extent by the choice of frequency and source type and the level of source and receiver in the two wells, such guided waves in cross-hole surveys may be important for monitoring changes in nearly horizontal reservoirs during hydrocarbon production processes. Initially, we investigate the basic properties of propagation in isotropic strata, and then examine the behaviour of guided waves in the stress-aligned fluid-filled inclusions. | ||
| 533 | |d 2006 |f Blackwell Publishing Journal Backfiles 1879-2005 |7 |2006|||||||||| | ||
| 700 | 1 | |a CRAMPIN, STUART |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i In |t Geophysical prospecting |d Oxford [u.a.] : Wiley-Blackwell, 1953 |g 41(1993), 3, Seite 0 |h Online-Ressource |w (DE-627)NLEJ243927630 |w (DE-600)2020311-1 |x 1365-2478 |7 nnns |
| 773 | 1 | 8 | |g volume:41 |g year:1993 |g number:3 |g pages:0 |
| 856 | 4 | 0 | |u http://dx.doi.org/10.1111/j.1365-2478.1993.tb00569.x |q text/html |x Verlag |z Deutschlandweit zugänglich |3 Volltext |
| 912 | |a GBV_USEFLAG_U | ||
| 912 | |a ZDB-1-DJB | ||
| 912 | |a GBV_NL_ARTICLE | ||
| 951 | |a AR | ||
| 952 | |d 41 |j 1993 |e 3 |h 0 | ||
| author_variant |
m l ml s c sc |
|---|---|
| matchkey_str |
article:13652478:1993----::oelngiewvsnrshlsresnnr |
| hierarchy_sort_str |
1993 |
| publishDate |
1993 |
| allfields |
10.1111/j.1365-2478.1993.tb00569.x doi (DE-627)NLEJ239605454 DE-627 ger DE-627 rakwb LOU, MIN verfasserin aut MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK Oxford, UK Blackwell Publishing Ltd 1993 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The theoretical behaviour of guided waves in cross-hole seismic surveys is examined with dispersion curves and synthetic seismograms. The modelling suggests, and field observations confirm, that the dominant energy in many cross-hole seismic surveys propagates as guided waves, as well as body waves, with the energy tied to an interface, or combination of interfaces, whenever there are interfaces with significant velocity contrasts continuous between the wells. The dispersion and waveforms of such modal solutions carry detailed information about the internal structure, particularly the stress-aligned structure of fluid-filled inclusions in the immediate neighbourhood of the waveguide. Since the information content can be controlled to some extent by the choice of frequency and source type and the level of source and receiver in the two wells, such guided waves in cross-hole surveys may be important for monitoring changes in nearly horizontal reservoirs during hydrocarbon production processes. Initially, we investigate the basic properties of propagation in isotropic strata, and then examine the behaviour of guided waves in the stress-aligned fluid-filled inclusions. 2006 Blackwell Publishing Journal Backfiles 1879-2005 |2006|||||||||| CRAMPIN, STUART verfasserin aut In Geophysical prospecting Oxford [u.a.] : Wiley-Blackwell, 1953 41(1993), 3, Seite 0 Online-Ressource (DE-627)NLEJ243927630 (DE-600)2020311-1 1365-2478 nnns volume:41 year:1993 number:3 pages:0 http://dx.doi.org/10.1111/j.1365-2478.1993.tb00569.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 41 1993 3 0 |
| spelling |
10.1111/j.1365-2478.1993.tb00569.x doi (DE-627)NLEJ239605454 DE-627 ger DE-627 rakwb LOU, MIN verfasserin aut MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK Oxford, UK Blackwell Publishing Ltd 1993 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The theoretical behaviour of guided waves in cross-hole seismic surveys is examined with dispersion curves and synthetic seismograms. The modelling suggests, and field observations confirm, that the dominant energy in many cross-hole seismic surveys propagates as guided waves, as well as body waves, with the energy tied to an interface, or combination of interfaces, whenever there are interfaces with significant velocity contrasts continuous between the wells. The dispersion and waveforms of such modal solutions carry detailed information about the internal structure, particularly the stress-aligned structure of fluid-filled inclusions in the immediate neighbourhood of the waveguide. Since the information content can be controlled to some extent by the choice of frequency and source type and the level of source and receiver in the two wells, such guided waves in cross-hole surveys may be important for monitoring changes in nearly horizontal reservoirs during hydrocarbon production processes. Initially, we investigate the basic properties of propagation in isotropic strata, and then examine the behaviour of guided waves in the stress-aligned fluid-filled inclusions. 2006 Blackwell Publishing Journal Backfiles 1879-2005 |2006|||||||||| CRAMPIN, STUART verfasserin aut In Geophysical prospecting Oxford [u.a.] : Wiley-Blackwell, 1953 41(1993), 3, Seite 0 Online-Ressource (DE-627)NLEJ243927630 (DE-600)2020311-1 1365-2478 nnns volume:41 year:1993 number:3 pages:0 http://dx.doi.org/10.1111/j.1365-2478.1993.tb00569.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 41 1993 3 0 |
| allfields_unstemmed |
10.1111/j.1365-2478.1993.tb00569.x doi (DE-627)NLEJ239605454 DE-627 ger DE-627 rakwb LOU, MIN verfasserin aut MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK Oxford, UK Blackwell Publishing Ltd 1993 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The theoretical behaviour of guided waves in cross-hole seismic surveys is examined with dispersion curves and synthetic seismograms. The modelling suggests, and field observations confirm, that the dominant energy in many cross-hole seismic surveys propagates as guided waves, as well as body waves, with the energy tied to an interface, or combination of interfaces, whenever there are interfaces with significant velocity contrasts continuous between the wells. The dispersion and waveforms of such modal solutions carry detailed information about the internal structure, particularly the stress-aligned structure of fluid-filled inclusions in the immediate neighbourhood of the waveguide. Since the information content can be controlled to some extent by the choice of frequency and source type and the level of source and receiver in the two wells, such guided waves in cross-hole surveys may be important for monitoring changes in nearly horizontal reservoirs during hydrocarbon production processes. Initially, we investigate the basic properties of propagation in isotropic strata, and then examine the behaviour of guided waves in the stress-aligned fluid-filled inclusions. 2006 Blackwell Publishing Journal Backfiles 1879-2005 |2006|||||||||| CRAMPIN, STUART verfasserin aut In Geophysical prospecting Oxford [u.a.] : Wiley-Blackwell, 1953 41(1993), 3, Seite 0 Online-Ressource (DE-627)NLEJ243927630 (DE-600)2020311-1 1365-2478 nnns volume:41 year:1993 number:3 pages:0 http://dx.doi.org/10.1111/j.1365-2478.1993.tb00569.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 41 1993 3 0 |
| allfieldsGer |
10.1111/j.1365-2478.1993.tb00569.x doi (DE-627)NLEJ239605454 DE-627 ger DE-627 rakwb LOU, MIN verfasserin aut MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK Oxford, UK Blackwell Publishing Ltd 1993 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The theoretical behaviour of guided waves in cross-hole seismic surveys is examined with dispersion curves and synthetic seismograms. The modelling suggests, and field observations confirm, that the dominant energy in many cross-hole seismic surveys propagates as guided waves, as well as body waves, with the energy tied to an interface, or combination of interfaces, whenever there are interfaces with significant velocity contrasts continuous between the wells. The dispersion and waveforms of such modal solutions carry detailed information about the internal structure, particularly the stress-aligned structure of fluid-filled inclusions in the immediate neighbourhood of the waveguide. Since the information content can be controlled to some extent by the choice of frequency and source type and the level of source and receiver in the two wells, such guided waves in cross-hole surveys may be important for monitoring changes in nearly horizontal reservoirs during hydrocarbon production processes. Initially, we investigate the basic properties of propagation in isotropic strata, and then examine the behaviour of guided waves in the stress-aligned fluid-filled inclusions. 2006 Blackwell Publishing Journal Backfiles 1879-2005 |2006|||||||||| CRAMPIN, STUART verfasserin aut In Geophysical prospecting Oxford [u.a.] : Wiley-Blackwell, 1953 41(1993), 3, Seite 0 Online-Ressource (DE-627)NLEJ243927630 (DE-600)2020311-1 1365-2478 nnns volume:41 year:1993 number:3 pages:0 http://dx.doi.org/10.1111/j.1365-2478.1993.tb00569.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 41 1993 3 0 |
| allfieldsSound |
10.1111/j.1365-2478.1993.tb00569.x doi (DE-627)NLEJ239605454 DE-627 ger DE-627 rakwb LOU, MIN verfasserin aut MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK Oxford, UK Blackwell Publishing Ltd 1993 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The theoretical behaviour of guided waves in cross-hole seismic surveys is examined with dispersion curves and synthetic seismograms. The modelling suggests, and field observations confirm, that the dominant energy in many cross-hole seismic surveys propagates as guided waves, as well as body waves, with the energy tied to an interface, or combination of interfaces, whenever there are interfaces with significant velocity contrasts continuous between the wells. The dispersion and waveforms of such modal solutions carry detailed information about the internal structure, particularly the stress-aligned structure of fluid-filled inclusions in the immediate neighbourhood of the waveguide. Since the information content can be controlled to some extent by the choice of frequency and source type and the level of source and receiver in the two wells, such guided waves in cross-hole surveys may be important for monitoring changes in nearly horizontal reservoirs during hydrocarbon production processes. Initially, we investigate the basic properties of propagation in isotropic strata, and then examine the behaviour of guided waves in the stress-aligned fluid-filled inclusions. 2006 Blackwell Publishing Journal Backfiles 1879-2005 |2006|||||||||| CRAMPIN, STUART verfasserin aut In Geophysical prospecting Oxford [u.a.] : Wiley-Blackwell, 1953 41(1993), 3, Seite 0 Online-Ressource (DE-627)NLEJ243927630 (DE-600)2020311-1 1365-2478 nnns volume:41 year:1993 number:3 pages:0 http://dx.doi.org/10.1111/j.1365-2478.1993.tb00569.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 41 1993 3 0 |
| source |
In Geophysical prospecting 41(1993), 3, Seite 0 volume:41 year:1993 number:3 pages:0 |
| sourceStr |
In Geophysical prospecting 41(1993), 3, Seite 0 volume:41 year:1993 number:3 pages:0 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| isfreeaccess_bool |
false |
| container_title |
Geophysical prospecting |
| authorswithroles_txt_mv |
LOU, MIN @@aut@@ CRAMPIN, STUART @@aut@@ |
| publishDateDaySort_date |
1993-01-01T00:00:00Z |
| hierarchy_top_id |
NLEJ243927630 |
| id |
NLEJ239605454 |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">NLEJ239605454</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20210707091538.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">120426s1993 xx |||||o 00| ||und c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1111/j.1365-2478.1993.tb00569.x</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)NLEJ239605454</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">LOU, MIN</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Oxford, UK</subfield><subfield code="b">Blackwell Publishing Ltd</subfield><subfield code="c">1993</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The theoretical behaviour of guided waves in cross-hole seismic surveys is examined with dispersion curves and synthetic seismograms. The modelling suggests, and field observations confirm, that the dominant energy in many cross-hole seismic surveys propagates as guided waves, as well as body waves, with the energy tied to an interface, or combination of interfaces, whenever there are interfaces with significant velocity contrasts continuous between the wells. The dispersion and waveforms of such modal solutions carry detailed information about the internal structure, particularly the stress-aligned structure of fluid-filled inclusions in the immediate neighbourhood of the waveguide. Since the information content can be controlled to some extent by the choice of frequency and source type and the level of source and receiver in the two wells, such guided waves in cross-hole surveys may be important for monitoring changes in nearly horizontal reservoirs during hydrocarbon production processes. Initially, we investigate the basic properties of propagation in isotropic strata, and then examine the behaviour of guided waves in the stress-aligned fluid-filled inclusions.</subfield></datafield><datafield tag="533" ind1=" " ind2=" "><subfield code="d">2006</subfield><subfield code="f">Blackwell Publishing Journal Backfiles 1879-2005</subfield><subfield code="7">|2006||||||||||</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">CRAMPIN, STUART</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Geophysical prospecting</subfield><subfield code="d">Oxford [u.a.] : Wiley-Blackwell, 1953</subfield><subfield code="g">41(1993), 3, Seite 0</subfield><subfield code="h">Online-Ressource</subfield><subfield code="w">(DE-627)NLEJ243927630</subfield><subfield code="w">(DE-600)2020311-1</subfield><subfield code="x">1365-2478</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:41</subfield><subfield code="g">year:1993</subfield><subfield code="g">number:3</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://dx.doi.org/10.1111/j.1365-2478.1993.tb00569.x</subfield><subfield code="q">text/html</subfield><subfield code="x">Verlag</subfield><subfield code="z">Deutschlandweit zugänglich</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-1-DJB</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_NL_ARTICLE</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">41</subfield><subfield code="j">1993</subfield><subfield code="e">3</subfield><subfield code="h">0</subfield></datafield></record></collection>
|
| series2 |
Blackwell Publishing Journal Backfiles 1879-2005 |
| author |
LOU, MIN |
| spellingShingle |
LOU, MIN MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK |
| authorStr |
LOU, MIN |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)NLEJ243927630 |
| format |
electronic Article |
| delete_txt_mv |
keep |
| author_role |
aut aut |
| collection |
NL |
| publishPlace |
Oxford, UK |
| remote_str |
true |
| illustrated |
Not Illustrated |
| issn |
1365-2478 |
| topic_title |
MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK |
| publisher |
Blackwell Publishing Ltd |
| publisherStr |
Blackwell Publishing Ltd |
| format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
zu |
| hierarchy_parent_title |
Geophysical prospecting |
| hierarchy_parent_id |
NLEJ243927630 |
| hierarchy_top_title |
Geophysical prospecting |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)NLEJ243927630 (DE-600)2020311-1 |
| title |
MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK |
| ctrlnum |
(DE-627)NLEJ239605454 |
| title_full |
MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK |
| author_sort |
LOU, MIN |
| journal |
Geophysical prospecting |
| journalStr |
Geophysical prospecting |
| isOA_bool |
false |
| recordtype |
marc |
| publishDateSort |
1993 |
| contenttype_str_mv |
zzz |
| container_start_page |
0 |
| author_browse |
LOU, MIN CRAMPIN, STUART |
| container_volume |
41 |
| physical |
Online-Ressource |
| format_se |
Elektronische Aufsätze |
| author-letter |
LOU, MIN |
| doi_str_mv |
10.1111/j.1365-2478.1993.tb00569.x |
| author2-role |
verfasserin |
| title_sort |
modelling guided waves in cross-hole surveys in uncracked and cracked rock |
| title_auth |
MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK |
| abstract |
The theoretical behaviour of guided waves in cross-hole seismic surveys is examined with dispersion curves and synthetic seismograms. The modelling suggests, and field observations confirm, that the dominant energy in many cross-hole seismic surveys propagates as guided waves, as well as body waves, with the energy tied to an interface, or combination of interfaces, whenever there are interfaces with significant velocity contrasts continuous between the wells. The dispersion and waveforms of such modal solutions carry detailed information about the internal structure, particularly the stress-aligned structure of fluid-filled inclusions in the immediate neighbourhood of the waveguide. Since the information content can be controlled to some extent by the choice of frequency and source type and the level of source and receiver in the two wells, such guided waves in cross-hole surveys may be important for monitoring changes in nearly horizontal reservoirs during hydrocarbon production processes. Initially, we investigate the basic properties of propagation in isotropic strata, and then examine the behaviour of guided waves in the stress-aligned fluid-filled inclusions. |
| abstractGer |
The theoretical behaviour of guided waves in cross-hole seismic surveys is examined with dispersion curves and synthetic seismograms. The modelling suggests, and field observations confirm, that the dominant energy in many cross-hole seismic surveys propagates as guided waves, as well as body waves, with the energy tied to an interface, or combination of interfaces, whenever there are interfaces with significant velocity contrasts continuous between the wells. The dispersion and waveforms of such modal solutions carry detailed information about the internal structure, particularly the stress-aligned structure of fluid-filled inclusions in the immediate neighbourhood of the waveguide. Since the information content can be controlled to some extent by the choice of frequency and source type and the level of source and receiver in the two wells, such guided waves in cross-hole surveys may be important for monitoring changes in nearly horizontal reservoirs during hydrocarbon production processes. Initially, we investigate the basic properties of propagation in isotropic strata, and then examine the behaviour of guided waves in the stress-aligned fluid-filled inclusions. |
| abstract_unstemmed |
The theoretical behaviour of guided waves in cross-hole seismic surveys is examined with dispersion curves and synthetic seismograms. The modelling suggests, and field observations confirm, that the dominant energy in many cross-hole seismic surveys propagates as guided waves, as well as body waves, with the energy tied to an interface, or combination of interfaces, whenever there are interfaces with significant velocity contrasts continuous between the wells. The dispersion and waveforms of such modal solutions carry detailed information about the internal structure, particularly the stress-aligned structure of fluid-filled inclusions in the immediate neighbourhood of the waveguide. Since the information content can be controlled to some extent by the choice of frequency and source type and the level of source and receiver in the two wells, such guided waves in cross-hole surveys may be important for monitoring changes in nearly horizontal reservoirs during hydrocarbon production processes. Initially, we investigate the basic properties of propagation in isotropic strata, and then examine the behaviour of guided waves in the stress-aligned fluid-filled inclusions. |
| collection_details |
GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE |
| container_issue |
3 |
| title_short |
MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK |
| url |
http://dx.doi.org/10.1111/j.1365-2478.1993.tb00569.x |
| remote_bool |
true |
| author2 |
CRAMPIN, STUART |
| author2Str |
CRAMPIN, STUART |
| ppnlink |
NLEJ243927630 |
| mediatype_str_mv |
z |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1111/j.1365-2478.1993.tb00569.x |
| up_date |
2024-07-06T07:53:10.929Z |
| _version_ |
1803815371072864256 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">NLEJ239605454</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20210707091538.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">120426s1993 xx |||||o 00| ||und c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1111/j.1365-2478.1993.tb00569.x</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)NLEJ239605454</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">LOU, MIN</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">MODELLING GUIDED WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Oxford, UK</subfield><subfield code="b">Blackwell Publishing Ltd</subfield><subfield code="c">1993</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The theoretical behaviour of guided waves in cross-hole seismic surveys is examined with dispersion curves and synthetic seismograms. The modelling suggests, and field observations confirm, that the dominant energy in many cross-hole seismic surveys propagates as guided waves, as well as body waves, with the energy tied to an interface, or combination of interfaces, whenever there are interfaces with significant velocity contrasts continuous between the wells. The dispersion and waveforms of such modal solutions carry detailed information about the internal structure, particularly the stress-aligned structure of fluid-filled inclusions in the immediate neighbourhood of the waveguide. Since the information content can be controlled to some extent by the choice of frequency and source type and the level of source and receiver in the two wells, such guided waves in cross-hole surveys may be important for monitoring changes in nearly horizontal reservoirs during hydrocarbon production processes. Initially, we investigate the basic properties of propagation in isotropic strata, and then examine the behaviour of guided waves in the stress-aligned fluid-filled inclusions.</subfield></datafield><datafield tag="533" ind1=" " ind2=" "><subfield code="d">2006</subfield><subfield code="f">Blackwell Publishing Journal Backfiles 1879-2005</subfield><subfield code="7">|2006||||||||||</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">CRAMPIN, STUART</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Geophysical prospecting</subfield><subfield code="d">Oxford [u.a.] : Wiley-Blackwell, 1953</subfield><subfield code="g">41(1993), 3, Seite 0</subfield><subfield code="h">Online-Ressource</subfield><subfield code="w">(DE-627)NLEJ243927630</subfield><subfield code="w">(DE-600)2020311-1</subfield><subfield code="x">1365-2478</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:41</subfield><subfield code="g">year:1993</subfield><subfield code="g">number:3</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://dx.doi.org/10.1111/j.1365-2478.1993.tb00569.x</subfield><subfield code="q">text/html</subfield><subfield code="x">Verlag</subfield><subfield code="z">Deutschlandweit zugänglich</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-1-DJB</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_NL_ARTICLE</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">41</subfield><subfield code="j">1993</subfield><subfield code="e">3</subfield><subfield code="h">0</subfield></datafield></record></collection>
|
| score |
7.4009247 |