Experimental Techniques in Mineral and Rock Physics: The Schreiber Volume
Knowledge of the relation between sonic velocity in sediments and rock lithology is one of the keys to interpreting data from seismic sections or from acoustic logs of sedimentary sequences. Reliable correlations of rock velocity with other petrophysical parameters, such as porosity or density, are...
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| Format: | Elektronisch E-Book |
| Sprache: | Englisch |
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Basel
Birkhäuser Basel
1994
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| Schriftenreihe: | Pageoph Topical Volumes
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| Links: | https://doi.org/10.1007/978-3-0348-5108-4 https://doi.org/10.1007/978-3-0348-5108-4 |
| Zusammenfassung: | Knowledge of the relation between sonic velocity in sediments and rock lithology is one of the keys to interpreting data from seismic sections or from acoustic logs of sedimentary sequences. Reliable correlations of rock velocity with other petrophysical parameters, such as porosity or density, are essential for calculating impedance models for synthetic seismic sections (BIDDLE et al. , 1992; CAMPBELL and STAFLEU, 1992) or identifying the origin of reflectivity on seismic lines (SELLAMI et al. , 1990; CHRISTENSEN and SZYMANSKI, 1991). Velocity is thus an important parameter for correlating lithological with geophysical data. Recent studies have increased our understanding of elastic rock properties in siliciclastic or shaly sediments. The causes for variations in velocity have been investigated for siliciclastic rocks (VERNIK and NUR, 1992), mixed carbonate siliciclastic sediments (CHRISTENSEN and SZYMANSKI, 1991), synthetic sand-clay mixtures (MARION et aI. , 1992) or claystones (JAPSEN, 1993). The concepts derived from these studies are however only partly applicable in pure carbonates. Carbon ates do not have large compositional variations that are, as is the case in the other sedimentary rocks, responsible for velocity contrasts. Pure carbonates are character ized by the lack of any clay or siliciclastic content, but are mostly produced and deposited on the top or on the slope of isolated or detached carbonate platforms, that have no hinterland as a source of terrigeneous material (WILSON, 1975; EBERLI, 1991) |
| Umfang: | 1 Online-Ressource (VII, 447 p. 110 illus) |
| ISBN: | 9783034851084 |
| DOI: | 10.1007/978-3-0348-5108-4 |
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| 520 | |a Knowledge of the relation between sonic velocity in sediments and rock lithology is one of the keys to interpreting data from seismic sections or from acoustic logs of sedimentary sequences. Reliable correlations of rock velocity with other petrophysical parameters, such as porosity or density, are essential for calculating impedance models for synthetic seismic sections (BIDDLE et al. , 1992; CAMPBELL and STAFLEU, 1992) or identifying the origin of reflectivity on seismic lines (SELLAMI et al. , 1990; CHRISTENSEN and SZYMANSKI, 1991). Velocity is thus an important parameter for correlating lithological with geophysical data. Recent studies have increased our understanding of elastic rock properties in siliciclastic or shaly sediments. The causes for variations in velocity have been investigated for siliciclastic rocks (VERNIK and NUR, 1992), mixed carbonate siliciclastic sediments (CHRISTENSEN and SZYMANSKI, 1991), synthetic sand-clay mixtures (MARION et aI. , 1992) or claystones (JAPSEN, 1993). The concepts derived from these studies are however only partly applicable in pure carbonates. Carbon ates do not have large compositional variations that are, as is the case in the other sedimentary rocks, responsible for velocity contrasts. Pure carbonates are character ized by the lack of any clay or siliciclastic content, but are mostly produced and deposited on the top or on the slope of isolated or detached carbonate platforms, that have no hinterland as a source of terrigeneous material (WILSON, 1975; EBERLI, 1991) | ||
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Datensatz im Suchindex
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| any_adam_object | |
| author2 | Liebermann, Robert C. Sondergeld, Carl H. |
| author2_role | edt edt |
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| author_facet | Liebermann, Robert C. Sondergeld, Carl H. |
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| ctrlnum | (ZDB-2-EES)978-3-0348-5108-4 (OCoLC)1053816141 (DE-599)BVBBV045177165 |
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| dewey-ones | 550 - Earth sciences 526 - Mathematical geography |
| dewey-raw | 550 526.1 |
| dewey-search | 550 526.1 |
| dewey-sort | 3550 |
| dewey-tens | 550 - Earth sciences 520 - Astronomy and allied sciences |
| discipline | Geologie / Paläontologie Physik |
| doi_str_mv | 10.1007/978-3-0348-5108-4 |
| format | Electronic eBook |
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| spelling | Experimental Techniques in Mineral and Rock Physics The Schreiber Volume edited by Robert C. Liebermann, Carl H. Sondergeld Reprint from Pure and Applied Geophysics (PAGEOPH), Volume 141 (1993), No. 2-4 Basel Birkhäuser Basel 1994 1 Online-Ressource (VII, 447 p. 110 illus) txt rdacontent c rdamedia cr rdacarrier Pageoph Topical Volumes Knowledge of the relation between sonic velocity in sediments and rock lithology is one of the keys to interpreting data from seismic sections or from acoustic logs of sedimentary sequences. Reliable correlations of rock velocity with other petrophysical parameters, such as porosity or density, are essential for calculating impedance models for synthetic seismic sections (BIDDLE et al. , 1992; CAMPBELL and STAFLEU, 1992) or identifying the origin of reflectivity on seismic lines (SELLAMI et al. , 1990; CHRISTENSEN and SZYMANSKI, 1991). Velocity is thus an important parameter for correlating lithological with geophysical data. Recent studies have increased our understanding of elastic rock properties in siliciclastic or shaly sediments. The causes for variations in velocity have been investigated for siliciclastic rocks (VERNIK and NUR, 1992), mixed carbonate siliciclastic sediments (CHRISTENSEN and SZYMANSKI, 1991), synthetic sand-clay mixtures (MARION et aI. , 1992) or claystones (JAPSEN, 1993). The concepts derived from these studies are however only partly applicable in pure carbonates. Carbon ates do not have large compositional variations that are, as is the case in the other sedimentary rocks, responsible for velocity contrasts. Pure carbonates are character ized by the lack of any clay or siliciclastic content, but are mostly produced and deposited on the top or on the slope of isolated or detached carbonate platforms, that have no hinterland as a source of terrigeneous material (WILSON, 1975; EBERLI, 1991) Schreiber, Edward 1930- (DE-588)119164604 gnd rswk-swf Earth Sciences Geophysics/Geodesy Geotechnical Engineering & Applied Earth Sciences Earth sciences Geophysics Geotechnical engineering Mineralogie (DE-588)4039457-8 gnd rswk-swf Gesteinskunde (DE-588)4020740-7 gnd rswk-swf Geophysik (DE-588)4020252-5 gnd rswk-swf Geochemie (DE-588)4020198-3 gnd rswk-swf (DE-588)1071861417 Konferenzschrift 1992 gnd-content (DE-588)4006432-3 Bibliografie gnd-content Gesteinskunde (DE-588)4020740-7 s Geophysik (DE-588)4020252-5 s DE-604 Mineralogie (DE-588)4039457-8 s Schreiber, Edward 1930- (DE-588)119164604 p Geochemie (DE-588)4020198-3 s Liebermann, Robert C. edt Sondergeld, Carl H. edt Erscheint auch als Druck-Ausgabe 9783764350284 https://doi.org/10.1007/978-3-0348-5108-4 Verlag URL des Erstveröffentlichers Volltext |
| spellingShingle | Experimental Techniques in Mineral and Rock Physics The Schreiber Volume Schreiber, Edward 1930- (DE-588)119164604 gnd Earth Sciences Geophysics/Geodesy Geotechnical Engineering & Applied Earth Sciences Earth sciences Geophysics Geotechnical engineering Mineralogie (DE-588)4039457-8 gnd Gesteinskunde (DE-588)4020740-7 gnd Geophysik (DE-588)4020252-5 gnd Geochemie (DE-588)4020198-3 gnd |
| subject_GND | (DE-588)119164604 (DE-588)4039457-8 (DE-588)4020740-7 (DE-588)4020252-5 (DE-588)4020198-3 (DE-588)1071861417 (DE-588)4006432-3 |
| title | Experimental Techniques in Mineral and Rock Physics The Schreiber Volume |
| title_alt | Reprint from Pure and Applied Geophysics (PAGEOPH), Volume 141 (1993), No. 2-4 |
| title_auth | Experimental Techniques in Mineral and Rock Physics The Schreiber Volume |
| title_exact_search | Experimental Techniques in Mineral and Rock Physics The Schreiber Volume |
| title_full | Experimental Techniques in Mineral and Rock Physics The Schreiber Volume edited by Robert C. Liebermann, Carl H. Sondergeld |
| title_fullStr | Experimental Techniques in Mineral and Rock Physics The Schreiber Volume edited by Robert C. Liebermann, Carl H. Sondergeld |
| title_full_unstemmed | Experimental Techniques in Mineral and Rock Physics The Schreiber Volume edited by Robert C. Liebermann, Carl H. Sondergeld |
| title_short | Experimental Techniques in Mineral and Rock Physics |
| title_sort | experimental techniques in mineral and rock physics the schreiber volume |
| title_sub | The Schreiber Volume |
| topic | Schreiber, Edward 1930- (DE-588)119164604 gnd Earth Sciences Geophysics/Geodesy Geotechnical Engineering & Applied Earth Sciences Earth sciences Geophysics Geotechnical engineering Mineralogie (DE-588)4039457-8 gnd Gesteinskunde (DE-588)4020740-7 gnd Geophysik (DE-588)4020252-5 gnd Geochemie (DE-588)4020198-3 gnd |
| topic_facet | Schreiber, Edward 1930- Earth Sciences Geophysics/Geodesy Geotechnical Engineering & Applied Earth Sciences Earth sciences Geophysics Geotechnical engineering Mineralogie Gesteinskunde Geophysik Geochemie Konferenzschrift 1992 Bibliografie |
| url | https://doi.org/10.1007/978-3-0348-5108-4 |
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