Principles of Applied Geophysics:
The welcome accorded to the first two editions of this book has been most encouraging. The object of the third edition continues to be to give a brief but "fairly comprehensive survey of the methods of applied geophysics including some of the modern interpretation techniques. The general approa...
Gespeichert in:
| 1. Verfasser: | |
|---|---|
| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Dordrecht
Springer Netherlands
1979
|
| Ausgabe: | Third Edition |
| Schlagworte: | |
| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | The welcome accorded to the first two editions of this book has been most encouraging. The object of the third edition continues to be to give a brief but "fairly comprehensive survey of the methods of applied geophysics including some of the modern interpretation techniques. The general approach and plan of the previous editions are preserved, but in bringing the book up to date some changes have been made to which I would like to draw the reader's special attention. SI units are strictly adhered to except in six illustrative figures reproduced from older literature and left intact to save some extensive redraughting. Following the recommendation of the International Union of Geodesy and Geophysics, the magnetic field measured in geophysical work is labelled here as flux density (tesla). Consequently, the symbols H, Z and T commonly used in geomagnetic work should stand for flux density. In the Max wellian theory of electromagnetism the symbol H stands, by convention, for a magnetizing force (A m -1) and a discerning reader will at once sense a source of confusion. This source of confusion is avoided in the present edition by B , B and B instead of H, Z and T. The employing the symbols b z t latter ~et is employed for the corresponding magnetizing forces of the earth's field. I hope this notation will gain general acceptance because it so easily dispenses with an ambiguity that otherwise tends to lead to unnecessary confusion of units and dimensions in geomagnetism |
| Beschreibung: | 1 Online-Ressource (X, 276 p) |
| ISBN: | 9789400958142 |
| DOI: | 10.1007/978-94-009-5814-2 |
Internformat
MARC
| LEADER | 00000nmm a2200000zc 4500 | ||
|---|---|---|---|
| 001 | BV045178573 | ||
| 003 | DE-604 | ||
| 005 | 00000000000000.0 | ||
| 007 | cr|uuu---uuuuu | ||
| 008 | 180911s1979 |||| o||u| ||||||eng d | ||
| 020 | |a 9789400958142 |9 978-94-009-5814-2 | ||
| 024 | 7 | |a 10.1007/978-94-009-5814-2 |2 doi | |
| 035 | |a (ZDB-2-EES)978-94-009-5814-2 | ||
| 035 | |a (OCoLC)1053823662 | ||
| 035 | |a (DE-599)BVBBV045178573 | ||
| 040 | |a DE-604 |b ger |e aacr | ||
| 041 | 0 | |a eng | |
| 049 | |a DE-634 | ||
| 082 | 0 | |a 526.1 |2 23 | |
| 082 | 0 | |a 550 |2 23 | |
| 084 | |a RB 10115 |0 (DE-625)142220:12621 |2 rvk | ||
| 100 | 1 | |a Parasnis, D. S. |e Verfasser |4 aut | |
| 245 | 1 | 0 | |a Principles of Applied Geophysics |c by D. S. Parasnis |
| 250 | |a Third Edition | ||
| 264 | 1 | |a Dordrecht |b Springer Netherlands |c 1979 | |
| 300 | |a 1 Online-Ressource (X, 276 p) | ||
| 336 | |b txt |2 rdacontent | ||
| 337 | |b c |2 rdamedia | ||
| 338 | |b cr |2 rdacarrier | ||
| 520 | |a The welcome accorded to the first two editions of this book has been most encouraging. The object of the third edition continues to be to give a brief but "fairly comprehensive survey of the methods of applied geophysics including some of the modern interpretation techniques. The general approach and plan of the previous editions are preserved, but in bringing the book up to date some changes have been made to which I would like to draw the reader's special attention. SI units are strictly adhered to except in six illustrative figures reproduced from older literature and left intact to save some extensive redraughting. Following the recommendation of the International Union of Geodesy and Geophysics, the magnetic field measured in geophysical work is labelled here as flux density (tesla). Consequently, the symbols H, Z and T commonly used in geomagnetic work should stand for flux density. In the Max wellian theory of electromagnetism the symbol H stands, by convention, for a magnetizing force (A m -1) and a discerning reader will at once sense a source of confusion. This source of confusion is avoided in the present edition by B , B and B instead of H, Z and T. The employing the symbols b z t latter ~et is employed for the corresponding magnetizing forces of the earth's field. I hope this notation will gain general acceptance because it so easily dispenses with an ambiguity that otherwise tends to lead to unnecessary confusion of units and dimensions in geomagnetism | ||
| 650 | 4 | |a Earth Sciences | |
| 650 | 4 | |a Geophysics/Geodesy | |
| 650 | 4 | |a Geophysics and Environmental Physics | |
| 650 | 4 | |a Science, general | |
| 650 | 4 | |a Earth sciences | |
| 650 | 4 | |a Science | |
| 650 | 4 | |a Geophysics | |
| 650 | 0 | 7 | |a Geophysik |0 (DE-588)4020252-5 |2 gnd |9 rswk-swf |
| 650 | 0 | 7 | |a Angewandte Geophysik |0 (DE-588)4122049-3 |2 gnd |9 rswk-swf |
| 650 | 0 | 7 | |a Methode |0 (DE-588)4038971-6 |2 gnd |9 rswk-swf |
| 689 | 0 | 0 | |a Geophysik |0 (DE-588)4020252-5 |D s |
| 689 | 0 | 1 | |a Methode |0 (DE-588)4038971-6 |D s |
| 689 | 0 | |5 DE-604 | |
| 689 | 1 | 0 | |a Angewandte Geophysik |0 (DE-588)4122049-3 |D s |
| 689 | 1 | |8 1\p |5 DE-604 | |
| 776 | 0 | 8 | |i Erscheint auch als |n Druck-Ausgabe |z 9780412158100 |
| 856 | 4 | 0 | |u https://doi.org/10.1007/978-94-009-5814-2 |x Verlag |z URL des Erstveröffentlichers |3 Volltext |
| 912 | |a ZDB-2-EES | ||
| 940 | 1 | |q ZDB-2-EES_Archiv | |
| 999 | |a oai:aleph.bib-bvb.de:BVB01-030567802 | ||
| 883 | 1 | |8 1\p |a cgwrk |d 20201028 |q DE-101 |u https://d-nb.info/provenance/plan#cgwrk | |
| 966 | e | |u https://doi.org/10.1007/978-94-009-5814-2 |l BTU01 |p ZDB-2-EES |q ZDB-2-EES_Archiv |x Verlag |3 Volltext | |
Datensatz im Suchindex
| _version_ | 1804178868999815168 |
|---|---|
| any_adam_object | |
| author | Parasnis, D. S. |
| author_facet | Parasnis, D. S. |
| author_role | aut |
| author_sort | Parasnis, D. S. |
| author_variant | d s p ds dsp |
| building | Verbundindex |
| bvnumber | BV045178573 |
| classification_rvk | RB 10115 |
| collection | ZDB-2-EES |
| ctrlnum | (ZDB-2-EES)978-94-009-5814-2 (OCoLC)1053823662 (DE-599)BVBBV045178573 |
| dewey-full | 526.1 550 |
| dewey-hundreds | 500 - Natural sciences and mathematics |
| dewey-ones | 526 - Mathematical geography 550 - Earth sciences |
| dewey-raw | 526.1 550 |
| dewey-search | 526.1 550 |
| dewey-sort | 3526.1 |
| dewey-tens | 520 - Astronomy and allied sciences 550 - Earth sciences |
| discipline | Physik Geologie / Paläontologie Geographie |
| doi_str_mv | 10.1007/978-94-009-5814-2 |
| edition | Third Edition |
| format | Electronic eBook |
| fullrecord | <?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>03524nmm a2200589zc 4500</leader><controlfield tag="001">BV045178573</controlfield><controlfield tag="003">DE-604</controlfield><controlfield tag="005">00000000000000.0</controlfield><controlfield tag="007">cr|uuu---uuuuu</controlfield><controlfield tag="008">180911s1979 |||| o||u| ||||||eng d</controlfield><datafield tag="020" ind1=" " ind2=" "><subfield code="a">9789400958142</subfield><subfield code="9">978-94-009-5814-2</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/978-94-009-5814-2</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ZDB-2-EES)978-94-009-5814-2</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)1053823662</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)BVBBV045178573</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-604</subfield><subfield code="b">ger</subfield><subfield code="e">aacr</subfield></datafield><datafield tag="041" ind1="0" ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="049" ind1=" " ind2=" "><subfield code="a">DE-634</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">526.1</subfield><subfield code="2">23</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">550</subfield><subfield code="2">23</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RB 10115</subfield><subfield code="0">(DE-625)142220:12621</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Parasnis, D. S.</subfield><subfield code="e">Verfasser</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Principles of Applied Geophysics</subfield><subfield code="c">by D. S. Parasnis</subfield></datafield><datafield tag="250" ind1=" " ind2=" "><subfield code="a">Third Edition</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Dordrecht</subfield><subfield code="b">Springer Netherlands</subfield><subfield code="c">1979</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (X, 276 p)</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The welcome accorded to the first two editions of this book has been most encouraging. The object of the third edition continues to be to give a brief but "fairly comprehensive survey of the methods of applied geophysics including some of the modern interpretation techniques. The general approach and plan of the previous editions are preserved, but in bringing the book up to date some changes have been made to which I would like to draw the reader's special attention. SI units are strictly adhered to except in six illustrative figures reproduced from older literature and left intact to save some extensive redraughting. Following the recommendation of the International Union of Geodesy and Geophysics, the magnetic field measured in geophysical work is labelled here as flux density (tesla). Consequently, the symbols H, Z and T commonly used in geomagnetic work should stand for flux density. In the Max wellian theory of electromagnetism the symbol H stands, by convention, for a magnetizing force (A m -1) and a discerning reader will at once sense a source of confusion. This source of confusion is avoided in the present edition by B , B and B instead of H, Z and T. The employing the symbols b z t latter ~et is employed for the corresponding magnetizing forces of the earth's field. I hope this notation will gain general acceptance because it so easily dispenses with an ambiguity that otherwise tends to lead to unnecessary confusion of units and dimensions in geomagnetism</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth Sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geophysics/Geodesy</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geophysics and Environmental Physics</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Science, general</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Science</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geophysics</subfield></datafield><datafield tag="650" ind1="0" ind2="7"><subfield code="a">Geophysik</subfield><subfield code="0">(DE-588)4020252-5</subfield><subfield code="2">gnd</subfield><subfield code="9">rswk-swf</subfield></datafield><datafield tag="650" ind1="0" ind2="7"><subfield code="a">Angewandte Geophysik</subfield><subfield code="0">(DE-588)4122049-3</subfield><subfield code="2">gnd</subfield><subfield code="9">rswk-swf</subfield></datafield><datafield tag="650" ind1="0" ind2="7"><subfield code="a">Methode</subfield><subfield code="0">(DE-588)4038971-6</subfield><subfield code="2">gnd</subfield><subfield code="9">rswk-swf</subfield></datafield><datafield tag="689" ind1="0" ind2="0"><subfield code="a">Geophysik</subfield><subfield code="0">(DE-588)4020252-5</subfield><subfield code="D">s</subfield></datafield><datafield tag="689" ind1="0" ind2="1"><subfield code="a">Methode</subfield><subfield code="0">(DE-588)4038971-6</subfield><subfield code="D">s</subfield></datafield><datafield tag="689" ind1="0" ind2=" "><subfield code="5">DE-604</subfield></datafield><datafield tag="689" ind1="1" ind2="0"><subfield code="a">Angewandte Geophysik</subfield><subfield code="0">(DE-588)4122049-3</subfield><subfield code="D">s</subfield></datafield><datafield tag="689" ind1="1" ind2=" "><subfield code="8">1\p</subfield><subfield code="5">DE-604</subfield></datafield><datafield tag="776" ind1="0" ind2="8"><subfield code="i">Erscheint auch als</subfield><subfield code="n">Druck-Ausgabe</subfield><subfield code="z">9780412158100</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1007/978-94-009-5814-2</subfield><subfield code="x">Verlag</subfield><subfield code="z">URL des Erstveröffentlichers</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-2-EES</subfield></datafield><datafield tag="940" ind1="1" ind2=" "><subfield code="q">ZDB-2-EES_Archiv</subfield></datafield><datafield tag="999" ind1=" " ind2=" "><subfield code="a">oai:aleph.bib-bvb.de:BVB01-030567802</subfield></datafield><datafield tag="883" ind1="1" ind2=" "><subfield code="8">1\p</subfield><subfield code="a">cgwrk</subfield><subfield code="d">20201028</subfield><subfield code="q">DE-101</subfield><subfield code="u">https://d-nb.info/provenance/plan#cgwrk</subfield></datafield><datafield tag="966" ind1="e" ind2=" "><subfield code="u">https://doi.org/10.1007/978-94-009-5814-2</subfield><subfield code="l">BTU01</subfield><subfield code="p">ZDB-2-EES</subfield><subfield code="q">ZDB-2-EES_Archiv</subfield><subfield code="x">Verlag</subfield><subfield code="3">Volltext</subfield></datafield></record></collection> |
| id | DE-604.BV045178573 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:49Z |
| institution | BVB |
| isbn | 9789400958142 |
| language | English |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-030567802 |
| oclc_num | 1053823662 |
| open_access_boolean | |
| owner | DE-634 |
| owner_facet | DE-634 |
| physical | 1 Online-Ressource (X, 276 p) |
| psigel | ZDB-2-EES ZDB-2-EES_Archiv ZDB-2-EES ZDB-2-EES_Archiv |
| publishDate | 1979 |
| publishDateSearch | 1979 |
| publishDateSort | 1979 |
| publisher | Springer Netherlands |
| record_format | marc |
| spelling | Parasnis, D. S. Verfasser aut Principles of Applied Geophysics by D. S. Parasnis Third Edition Dordrecht Springer Netherlands 1979 1 Online-Ressource (X, 276 p) txt rdacontent c rdamedia cr rdacarrier The welcome accorded to the first two editions of this book has been most encouraging. The object of the third edition continues to be to give a brief but "fairly comprehensive survey of the methods of applied geophysics including some of the modern interpretation techniques. The general approach and plan of the previous editions are preserved, but in bringing the book up to date some changes have been made to which I would like to draw the reader's special attention. SI units are strictly adhered to except in six illustrative figures reproduced from older literature and left intact to save some extensive redraughting. Following the recommendation of the International Union of Geodesy and Geophysics, the magnetic field measured in geophysical work is labelled here as flux density (tesla). Consequently, the symbols H, Z and T commonly used in geomagnetic work should stand for flux density. In the Max wellian theory of electromagnetism the symbol H stands, by convention, for a magnetizing force (A m -1) and a discerning reader will at once sense a source of confusion. This source of confusion is avoided in the present edition by B , B and B instead of H, Z and T. The employing the symbols b z t latter ~et is employed for the corresponding magnetizing forces of the earth's field. I hope this notation will gain general acceptance because it so easily dispenses with an ambiguity that otherwise tends to lead to unnecessary confusion of units and dimensions in geomagnetism Earth Sciences Geophysics/Geodesy Geophysics and Environmental Physics Science, general Earth sciences Science Geophysics Geophysik (DE-588)4020252-5 gnd rswk-swf Angewandte Geophysik (DE-588)4122049-3 gnd rswk-swf Methode (DE-588)4038971-6 gnd rswk-swf Geophysik (DE-588)4020252-5 s Methode (DE-588)4038971-6 s DE-604 Angewandte Geophysik (DE-588)4122049-3 s 1\p DE-604 Erscheint auch als Druck-Ausgabe 9780412158100 https://doi.org/10.1007/978-94-009-5814-2 Verlag URL des Erstveröffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
| spellingShingle | Parasnis, D. S. Principles of Applied Geophysics Earth Sciences Geophysics/Geodesy Geophysics and Environmental Physics Science, general Earth sciences Science Geophysics Geophysik (DE-588)4020252-5 gnd Angewandte Geophysik (DE-588)4122049-3 gnd Methode (DE-588)4038971-6 gnd |
| subject_GND | (DE-588)4020252-5 (DE-588)4122049-3 (DE-588)4038971-6 |
| title | Principles of Applied Geophysics |
| title_auth | Principles of Applied Geophysics |
| title_exact_search | Principles of Applied Geophysics |
| title_full | Principles of Applied Geophysics by D. S. Parasnis |
| title_fullStr | Principles of Applied Geophysics by D. S. Parasnis |
| title_full_unstemmed | Principles of Applied Geophysics by D. S. Parasnis |
| title_short | Principles of Applied Geophysics |
| title_sort | principles of applied geophysics |
| topic | Earth Sciences Geophysics/Geodesy Geophysics and Environmental Physics Science, general Earth sciences Science Geophysics Geophysik (DE-588)4020252-5 gnd Angewandte Geophysik (DE-588)4122049-3 gnd Methode (DE-588)4038971-6 gnd |
| topic_facet | Earth Sciences Geophysics/Geodesy Geophysics and Environmental Physics Science, general Earth sciences Science Geophysics Geophysik Angewandte Geophysik Methode |
| url | https://doi.org/10.1007/978-94-009-5814-2 |
| work_keys_str_mv | AT parasnisds principlesofappliedgeophysics |