The Mid-Oceanic Ridges: Mountains Below Sea Level
Over the past 20 years, geologists have come to realize that the real object of their studies is the Earth, and that their favorite subjects, whether basalts, earthquakes, or the Tibetan plateau (for example) are only the means to understanding the Earth itself as a complete entity. Geology has thus...
Gespeichert in:
| 1. Verfasser: | |
|---|---|
| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Berlin, Heidelberg
Springer Berlin Heidelberg
1995
|
| Schlagworte: | |
| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | Over the past 20 years, geologists have come to realize that the real object of their studies is the Earth, and that their favorite subjects, whether basalts, earthquakes, or the Tibetan plateau (for example) are only the means to understanding the Earth itself as a complete entity. Geology has thus acquired aglobai perspective. The study of any particular regional problem is only of general interest in providing good foundations to investigate general phe nomena. But this same particular problem can only be completely understood ifits global context is taken into account. The geology of the Andes is only one of many examples of subcontinental subduc tion and, as such, its study contributes to our understanding of the mechanism of subduction. However, at the same time, understanding the geology of the Andes is today no longer possible without relating it to the geological history of the eastern Pacific, reconstructing the relative movements of the East Pacific Rise and the Nazca Ridge against South America and, in a wider sense, in the context of the his tory of the Pacific Ocean as a whole. Geology today is based on an infinite variety of natural examples which in the general frame of plate tectonics deals with geometrie objects, historie situations, or the various methods employed. The object "Earth" includes not only subjects like seismology, structural geology, and geochemistry, but also studies of the crust, mantle and core, oceans and continents, and mountain ranges and basins |
| Beschreibung: | 1 Online-Ressource (XVII, 201 p. 174 illus., 103 illus. in color) |
| ISBN: | 9783662031360 |
| DOI: | 10.1007/978-3-662-03136-0 |
Internformat
MARC
| LEADER | 00000nmm a2200000zc 4500 | ||
|---|---|---|---|
| 001 | BV045178283 | ||
| 003 | DE-604 | ||
| 005 | 20200520 | ||
| 007 | cr|uuu---uuuuu | ||
| 008 | 180911s1995 |||| o||u| ||||||eng d | ||
| 020 | |a 9783662031360 |9 978-3-662-03136-0 | ||
| 024 | 7 | |a 10.1007/978-3-662-03136-0 |2 doi | |
| 035 | |a (ZDB-2-EES)978-3-662-03136-0 | ||
| 035 | |a (OCoLC)1053823306 | ||
| 035 | |a (DE-599)BVBBV045178283 | ||
| 040 | |a DE-604 |b ger |e aacr | ||
| 041 | 0 | |a eng | |
| 049 | |a DE-634 | ||
| 082 | 0 | |a 551 |2 23 | |
| 084 | |a RZ 10121 |0 (DE-625)142561:12623 |2 rvk | ||
| 100 | 1 | |a Nicolas, Adolphe |d 1936-2020 |e Verfasser |0 (DE-588)1089202954 |4 aut | |
| 245 | 1 | 0 | |a The Mid-Oceanic Ridges |b Mountains Below Sea Level |c by Adolphe Nicolas |
| 264 | 1 | |a Berlin, Heidelberg |b Springer Berlin Heidelberg |c 1995 | |
| 300 | |a 1 Online-Ressource (XVII, 201 p. 174 illus., 103 illus. in color) | ||
| 336 | |b txt |2 rdacontent | ||
| 337 | |b c |2 rdamedia | ||
| 338 | |b cr |2 rdacarrier | ||
| 520 | |a Over the past 20 years, geologists have come to realize that the real object of their studies is the Earth, and that their favorite subjects, whether basalts, earthquakes, or the Tibetan plateau (for example) are only the means to understanding the Earth itself as a complete entity. Geology has thus acquired aglobai perspective. The study of any particular regional problem is only of general interest in providing good foundations to investigate general phe nomena. But this same particular problem can only be completely understood ifits global context is taken into account. The geology of the Andes is only one of many examples of subcontinental subduc tion and, as such, its study contributes to our understanding of the mechanism of subduction. However, at the same time, understanding the geology of the Andes is today no longer possible without relating it to the geological history of the eastern Pacific, reconstructing the relative movements of the East Pacific Rise and the Nazca Ridge against South America and, in a wider sense, in the context of the his tory of the Pacific Ocean as a whole. Geology today is based on an infinite variety of natural examples which in the general frame of plate tectonics deals with geometrie objects, historie situations, or the various methods employed. The object "Earth" includes not only subjects like seismology, structural geology, and geochemistry, but also studies of the crust, mantle and core, oceans and continents, and mountain ranges and basins | ||
| 650 | 4 | |a Earth Sciences | |
| 650 | 4 | |a Geology | |
| 650 | 4 | |a Oceanography | |
| 650 | 4 | |a Mineralogy | |
| 650 | 4 | |a Earth sciences | |
| 650 | 4 | |a Geology | |
| 650 | 4 | |a Mineralogy | |
| 650 | 4 | |a Oceanography | |
| 650 | 0 | 7 | |a Ozeanischer Rücken |0 (DE-588)4368695-3 |2 gnd |9 rswk-swf |
| 650 | 0 | 7 | |a Plattentektonik |0 (DE-588)4046317-5 |2 gnd |9 rswk-swf |
| 650 | 0 | 7 | |a Magmatisches Gestein |0 (DE-588)4036974-2 |2 gnd |9 rswk-swf |
| 651 | 7 | |a Mittelozeanischer Rücken |0 (DE-588)4317501-6 |2 gnd |9 rswk-swf | |
| 689 | 0 | 0 | |a Mittelozeanischer Rücken |0 (DE-588)4317501-6 |D g |
| 689 | 0 | 1 | |a Magmatisches Gestein |0 (DE-588)4036974-2 |D s |
| 689 | 0 | |5 DE-604 | |
| 689 | 1 | 0 | |a Plattentektonik |0 (DE-588)4046317-5 |D s |
| 689 | 1 | 1 | |a Mittelozeanischer Rücken |0 (DE-588)4317501-6 |D g |
| 689 | 1 | |5 DE-604 | |
| 689 | 2 | 0 | |a Ozeanischer Rücken |0 (DE-588)4368695-3 |D s |
| 689 | 2 | |5 DE-604 | |
| 776 | 0 | 8 | |i Erscheint auch als |n Druck-Ausgabe |z 9783540573807 |
| 856 | 4 | 0 | |u https://doi.org/10.1007/978-3-662-03136-0 |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:BVB01-030567513 | ||
| 966 | e | |u https://doi.org/10.1007/978-3-662-03136-0 |l BTU01 |p ZDB-2-EES |q ZDB-2-EES_Archiv |x Verlag |3 Volltext | |
Datensatz im Suchindex
| _version_ | 1804178868351795200 |
|---|---|
| any_adam_object | |
| author | Nicolas, Adolphe 1936-2020 |
| author_GND | (DE-588)1089202954 |
| author_facet | Nicolas, Adolphe 1936-2020 |
| author_role | aut |
| author_sort | Nicolas, Adolphe 1936-2020 |
| author_variant | a n an |
| building | Verbundindex |
| bvnumber | BV045178283 |
| classification_rvk | RZ 10121 |
| collection | ZDB-2-EES |
| ctrlnum | (ZDB-2-EES)978-3-662-03136-0 (OCoLC)1053823306 (DE-599)BVBBV045178283 |
| dewey-full | 551 |
| dewey-hundreds | 500 - Natural sciences and mathematics |
| dewey-ones | 551 - Geology, hydrology, meteorology |
| dewey-raw | 551 |
| dewey-search | 551 |
| dewey-sort | 3551 |
| dewey-tens | 550 - Earth sciences |
| discipline | Geologie / Paläontologie Geographie |
| doi_str_mv | 10.1007/978-3-662-03136-0 |
| format | Electronic eBook |
| fullrecord | <?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>03750nmm a2200613zc 4500</leader><controlfield tag="001">BV045178283</controlfield><controlfield tag="003">DE-604</controlfield><controlfield tag="005">20200520 </controlfield><controlfield tag="007">cr|uuu---uuuuu</controlfield><controlfield tag="008">180911s1995 |||| o||u| ||||||eng d</controlfield><datafield tag="020" ind1=" " ind2=" "><subfield code="a">9783662031360</subfield><subfield code="9">978-3-662-03136-0</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/978-3-662-03136-0</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ZDB-2-EES)978-3-662-03136-0</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)1053823306</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)BVBBV045178283</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">551</subfield><subfield code="2">23</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RZ 10121</subfield><subfield code="0">(DE-625)142561:12623</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Nicolas, Adolphe</subfield><subfield code="d">1936-2020</subfield><subfield code="e">Verfasser</subfield><subfield code="0">(DE-588)1089202954</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">The Mid-Oceanic Ridges</subfield><subfield code="b">Mountains Below Sea Level</subfield><subfield code="c">by Adolphe Nicolas</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Berlin, Heidelberg</subfield><subfield code="b">Springer Berlin Heidelberg</subfield><subfield code="c">1995</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (XVII, 201 p. 174 illus., 103 illus. in color)</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">Over the past 20 years, geologists have come to realize that the real object of their studies is the Earth, and that their favorite subjects, whether basalts, earthquakes, or the Tibetan plateau (for example) are only the means to understanding the Earth itself as a complete entity. Geology has thus acquired aglobai perspective. The study of any particular regional problem is only of general interest in providing good foundations to investigate general phe nomena. But this same particular problem can only be completely understood ifits global context is taken into account. The geology of the Andes is only one of many examples of subcontinental subduc tion and, as such, its study contributes to our understanding of the mechanism of subduction. However, at the same time, understanding the geology of the Andes is today no longer possible without relating it to the geological history of the eastern Pacific, reconstructing the relative movements of the East Pacific Rise and the Nazca Ridge against South America and, in a wider sense, in the context of the his tory of the Pacific Ocean as a whole. Geology today is based on an infinite variety of natural examples which in the general frame of plate tectonics deals with geometrie objects, historie situations, or the various methods employed. The object "Earth" includes not only subjects like seismology, structural geology, and geochemistry, but also studies of the crust, mantle and core, oceans and continents, and mountain ranges and basins</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth Sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Oceanography</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mineralogy</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mineralogy</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Oceanography</subfield></datafield><datafield tag="650" ind1="0" ind2="7"><subfield code="a">Ozeanischer Rücken</subfield><subfield code="0">(DE-588)4368695-3</subfield><subfield code="2">gnd</subfield><subfield code="9">rswk-swf</subfield></datafield><datafield tag="650" ind1="0" ind2="7"><subfield code="a">Plattentektonik</subfield><subfield code="0">(DE-588)4046317-5</subfield><subfield code="2">gnd</subfield><subfield code="9">rswk-swf</subfield></datafield><datafield tag="650" ind1="0" ind2="7"><subfield code="a">Magmatisches Gestein</subfield><subfield code="0">(DE-588)4036974-2</subfield><subfield code="2">gnd</subfield><subfield code="9">rswk-swf</subfield></datafield><datafield tag="651" ind1=" " ind2="7"><subfield code="a">Mittelozeanischer Rücken</subfield><subfield code="0">(DE-588)4317501-6</subfield><subfield code="2">gnd</subfield><subfield code="9">rswk-swf</subfield></datafield><datafield tag="689" ind1="0" ind2="0"><subfield code="a">Mittelozeanischer Rücken</subfield><subfield code="0">(DE-588)4317501-6</subfield><subfield code="D">g</subfield></datafield><datafield tag="689" ind1="0" ind2="1"><subfield code="a">Magmatisches Gestein</subfield><subfield code="0">(DE-588)4036974-2</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">Plattentektonik</subfield><subfield code="0">(DE-588)4046317-5</subfield><subfield code="D">s</subfield></datafield><datafield tag="689" ind1="1" ind2="1"><subfield code="a">Mittelozeanischer Rücken</subfield><subfield code="0">(DE-588)4317501-6</subfield><subfield code="D">g</subfield></datafield><datafield tag="689" ind1="1" ind2=" "><subfield code="5">DE-604</subfield></datafield><datafield tag="689" ind1="2" ind2="0"><subfield code="a">Ozeanischer Rücken</subfield><subfield code="0">(DE-588)4368695-3</subfield><subfield code="D">s</subfield></datafield><datafield tag="689" ind1="2" ind2=" "><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">9783540573807</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1007/978-3-662-03136-0</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:BVB01-030567513</subfield></datafield><datafield tag="966" ind1="e" ind2=" "><subfield code="u">https://doi.org/10.1007/978-3-662-03136-0</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> |
| geographic | Mittelozeanischer Rücken (DE-588)4317501-6 gnd |
| geographic_facet | Mittelozeanischer Rücken |
| id | DE-604.BV045178283 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:48Z |
| institution | BVB |
| isbn | 9783662031360 |
| language | English |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-030567513 |
| oclc_num | 1053823306 |
| open_access_boolean | |
| owner | DE-634 |
| owner_facet | DE-634 |
| physical | 1 Online-Ressource (XVII, 201 p. 174 illus., 103 illus. in color) |
| psigel | ZDB-2-EES ZDB-2-EES_Archiv ZDB-2-EES ZDB-2-EES_Archiv |
| publishDate | 1995 |
| publishDateSearch | 1995 |
| publishDateSort | 1995 |
| publisher | Springer Berlin Heidelberg |
| record_format | marc |
| spelling | Nicolas, Adolphe 1936-2020 Verfasser (DE-588)1089202954 aut The Mid-Oceanic Ridges Mountains Below Sea Level by Adolphe Nicolas Berlin, Heidelberg Springer Berlin Heidelberg 1995 1 Online-Ressource (XVII, 201 p. 174 illus., 103 illus. in color) txt rdacontent c rdamedia cr rdacarrier Over the past 20 years, geologists have come to realize that the real object of their studies is the Earth, and that their favorite subjects, whether basalts, earthquakes, or the Tibetan plateau (for example) are only the means to understanding the Earth itself as a complete entity. Geology has thus acquired aglobai perspective. The study of any particular regional problem is only of general interest in providing good foundations to investigate general phe nomena. But this same particular problem can only be completely understood ifits global context is taken into account. The geology of the Andes is only one of many examples of subcontinental subduc tion and, as such, its study contributes to our understanding of the mechanism of subduction. However, at the same time, understanding the geology of the Andes is today no longer possible without relating it to the geological history of the eastern Pacific, reconstructing the relative movements of the East Pacific Rise and the Nazca Ridge against South America and, in a wider sense, in the context of the his tory of the Pacific Ocean as a whole. Geology today is based on an infinite variety of natural examples which in the general frame of plate tectonics deals with geometrie objects, historie situations, or the various methods employed. The object "Earth" includes not only subjects like seismology, structural geology, and geochemistry, but also studies of the crust, mantle and core, oceans and continents, and mountain ranges and basins Earth Sciences Geology Oceanography Mineralogy Earth sciences Ozeanischer Rücken (DE-588)4368695-3 gnd rswk-swf Plattentektonik (DE-588)4046317-5 gnd rswk-swf Magmatisches Gestein (DE-588)4036974-2 gnd rswk-swf Mittelozeanischer Rücken (DE-588)4317501-6 gnd rswk-swf Mittelozeanischer Rücken (DE-588)4317501-6 g Magmatisches Gestein (DE-588)4036974-2 s DE-604 Plattentektonik (DE-588)4046317-5 s Ozeanischer Rücken (DE-588)4368695-3 s Erscheint auch als Druck-Ausgabe 9783540573807 https://doi.org/10.1007/978-3-662-03136-0 Verlag URL des Erstveröffentlichers Volltext |
| spellingShingle | Nicolas, Adolphe 1936-2020 The Mid-Oceanic Ridges Mountains Below Sea Level Earth Sciences Geology Oceanography Mineralogy Earth sciences Ozeanischer Rücken (DE-588)4368695-3 gnd Plattentektonik (DE-588)4046317-5 gnd Magmatisches Gestein (DE-588)4036974-2 gnd |
| subject_GND | (DE-588)4368695-3 (DE-588)4046317-5 (DE-588)4036974-2 (DE-588)4317501-6 |
| title | The Mid-Oceanic Ridges Mountains Below Sea Level |
| title_auth | The Mid-Oceanic Ridges Mountains Below Sea Level |
| title_exact_search | The Mid-Oceanic Ridges Mountains Below Sea Level |
| title_full | The Mid-Oceanic Ridges Mountains Below Sea Level by Adolphe Nicolas |
| title_fullStr | The Mid-Oceanic Ridges Mountains Below Sea Level by Adolphe Nicolas |
| title_full_unstemmed | The Mid-Oceanic Ridges Mountains Below Sea Level by Adolphe Nicolas |
| title_short | The Mid-Oceanic Ridges |
| title_sort | the mid oceanic ridges mountains below sea level |
| title_sub | Mountains Below Sea Level |
| topic | Earth Sciences Geology Oceanography Mineralogy Earth sciences Ozeanischer Rücken (DE-588)4368695-3 gnd Plattentektonik (DE-588)4046317-5 gnd Magmatisches Gestein (DE-588)4036974-2 gnd |
| topic_facet | Earth Sciences Geology Oceanography Mineralogy Earth sciences Ozeanischer Rücken Plattentektonik Magmatisches Gestein Mittelozeanischer Rücken |
| url | https://doi.org/10.1007/978-3-662-03136-0 |
| work_keys_str_mv | AT nicolasadolphe themidoceanicridgesmountainsbelowsealevel |