The mid-oceanic ridges: mountains below sea level
Despite turbulent actions of plate tectonics, continents, which since the first cooling of the planet float on its substratum, are a geological record of the history of Earth. Since the existing oceans are geologically relatively young, they register the activity, the life of the Earth. They formed...
Gespeichert in:
| 1. Verfasser: | |
|---|---|
| Format: | Buch |
| Sprache: | German English French |
| Veröffentlicht: |
Berlin [u.a.]
Springer
1995
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| Schlagworte: | |
| Online-Zugang: | Inhaltsverzeichnis |
| Zusammenfassung: | Despite turbulent actions of plate tectonics, continents, which since the first cooling of the planet float on its substratum, are a geological record of the history of Earth. Since the existing oceans are geologically relatively young, they register the activity, the life of the Earth. They formed when a large supercontinent (Pangea) broke apart some 150 Ma ago. The mid-oceanic ridges are narrow belts of submarine mountains marking the boundaries between plates which are moving apart, with new oceanic crust being created at the same time. Under the continents oceanic crust is subducted. The ocean bottom is an ideal location to study recent geodynamic processes on Earth. Of special interest to the reader will be the combination of the most recent oceanographic data with ophiolites, representing fossil ocean crust, obducted onto the continents by tectonic processes. |
| Beschreibung: | Dt. Ausg. u.d.T.: Nicolas, Adolphe: Die ozeanischen Rücken |
| Beschreibung: | XVII, 200 S. Ill., graph. Darst., Kt. |
| ISBN: | 3540573801 0387573801 |
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| 245 | 1 | 0 | |a The mid-oceanic ridges |b mountains below sea level |c Adolphe Nicolas. [Transl.: Thomas Reimer] |
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| 520 | 3 | |a Despite turbulent actions of plate tectonics, continents, which since the first cooling of the planet float on its substratum, are a geological record of the history of Earth. Since the existing oceans are geologically relatively young, they register the activity, the life of the Earth. They formed when a large supercontinent (Pangea) broke apart some 150 Ma ago. The mid-oceanic ridges are narrow belts of submarine mountains marking the boundaries between plates which are moving apart, with new oceanic crust being created at the same time. Under the continents oceanic crust is subducted. The ocean bottom is an ideal location to study recent geodynamic processes on Earth. Of special interest to the reader will be the combination of the most recent oceanographic data with ophiolites, representing fossil ocean crust, obducted onto the continents by tectonic processes. | |
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Datensatz im Suchindex
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ADOLPHE NICOLAS THE MID-OCEANIC RIDGES MOUNTAINS BELOW SEA LEVEL WITH 92
FIGURES SPRINGER 1 YOUNG AND LIVING OCEANS 1 THE OPENING OF THE OCEANS -
PROOF OF GLOBAL TECTONICS 2 ZEBRA PATTERNS ON THE OCEAN FLOORS 2 PLATE
KINEMATICS - A CARTOON 6 THE SEDIMENTARY RECORD OF THE OPENING OF THE
OCEANS 10 LIFE AND DEATH OF THE OCEANS 10 THE FIRST SIGNS OF AGE 10
THERMAL SUBSIDENCE 11 MATURITY 15 OLD CONTINENTS AND YOUNG OCEANS 15 THE
MARINE CEMETERY 17 2 THE EARTH, A HEAT ENGINE 23 CONVECTION IN THE
MANTLE 25 THE CONVECTION CIRCUITS 25 GEOTHERMAL GRADIENTS AND CONVECTION
31 HOTSPOTS AND MANTLE PLUMES 34 THE CHEMICAL FINGERPRINT OF HOTSPOTS 39
ISOTOPE GEOCHEMISTRY AND MANTLE RESERVOIRS 40 THE ORIGIN OF HOTSPOTS 42
3 THE RIDGES - CRADLES OF THE OCEAN 45 SUBMARINE TOPOGRAPHY AND GEOLOGY
45 THE HIGHS AND LOWS OF THE OCEAN SURFACE 48 THE BELT OF RIFTS AND
RIDGES 52 FRACTURE ZONES 55 KINEMATICS ON A SPHERE 59 SLOW- AND
FAST-SPREADING RIDGES 61 SEGMENTATION OF THE RIDGES 61 OCEANIC AND
CONTINENTAL RIFTS 65 4 SUBMARINE EXPLORATION 69 THE OCEANIC ROCKS 69 XV
CONTENTS THE PENETRATING EYE OF GEOPHYSICS 73 GEOLOGISTS AND
GEOPHYSICISTS: SQUARE YOUR ACCOUNTS! 73 STRUCTURE OF THE OCEAN CRUST 73
RIDGE DYNAMICS 74 HYDROTHERMAL ACTIVITY OF RIDGES 77 APRIL 20TH, 1979 77
THE BLACK SMOKERS 79 MOUNTAINS COVERED BY CARBONATE SNOW 81 DID LIFE
ORIGINATE ON THE RIDGES? 82 5 OPHIOLITES - OR IN SEARCH OF LOST OCEANS
69 THE OCEAN, DRY-FOOTED 69 THE SNAKE ROCK 88 SAMPLING THE OCEANS 88
STRANDING OR OBDUCTION OF OPHIOLITES ON THE CONTINENTS 90 THE BEST
OPHIOLITE IN THE WORLD 91 THE LONG JOURNEY OF THE OMAN OPHIOLITES 93 THE
OPHIOLITES AS FRAGMENTS OF YOUNG OCEANIC LITHOSPHERE . . 97 COMPARATIVE
"OPHIOLITOLOGY" 99 OPHIOLITES DO NOT BELONG TO A UNIQUE SPECIES 99 THE
GEODYNAMIC ENVIRONMENT OF OPHIOLITES 100 THE FUNCTIONING OF THE RIDGES:
A STRUCTURAL PERSPECTIVE 101 THE OPHIOLITE PUZZLE AND ITS KEY 101 THE
TWO TYPES OF OPHIOLITES 104 LHERZOLITES AND HARZBURGITES 105 COMPARISON
OF THE CHARACTERISTICS OF THE TWO TYPES OF OPHIOLITES 107 6 MANTLE
METALLURGY ILL THE MESSAGE OF THE MANTLE ILL OPHIOLITES DEPRIVED OF
THEIR MANTLE ILL MANTLE METTALURGY 113 MOVING MANTLE UNDER THE RIDGES
117 A RULE OF CONDUCT 117 THE ROOTS OF VOLCANOES 119 MELTING OF MANTLE
119 THE EXTRACTION OF BASALT: FIELD EVIDENCE 122 MELT CAN FRACTURE THE
PERIDOTITE 125 EPISODIC NATURE AND VIOLENCE OF VOLCANISM 129 7 T H E
FORGES OF VULCAN IN T H E K I N G D O M OF N E P T U N E . 131
CONTINUOUS FLOW 131 A WELL-COMBED MANDE 133 XVI CONTENTS DIAPIRS -
MUSHROOMS UNDER THE RIDGE 135 CHIMNEYS IN THE MANTLE 139 THE FOCUSSING
EFFECT OF A RIDGE 141 IS THERE A MOHO BELOW A RIDGE? 142 THE ORIGIN OF A
CHROMITE DEPOSIT - A FREAK OF NATURE 146 FLATTENING OF A DIAPIR BELOW A
RIDGE 149 MAGMA CHAMBERS: LAYERED IGNEOUS COMPLEXES? 151 THE MAGMA
CHAMBERS BELOW RIDGES 152 THE CARAPACE OF RIDGES 155 THE RECONSTRUCTED
RIDGE 156 8 FROM RIFTS TO FAST-SPREADING RIDGES 159 SLOW- OR
FAST-SPREADING RIDGES AND OPHIOLITES 160 EXPANSION OF RIFTS 160
EXPANSION OF SLOW-SPREADING RIFFS 165 THE MOHO UNCOVERED 165 THE RHYTHMS
OF SLOW-SPREADING RIDGES 165 IS THE MOHO REALLY AT 6 KM? 169 IN SEARCH
OF A GENERAL MODEL 170 THE SIGNATURE OF THE MANTLE 171 THE WEDGE AND THE
MUSHROOM 173 LITHOSPHERIC UNDERPLATING 173 MANTLE DIAPIRISM AS THE CAUSE
OF SEGMENTATION AND PERIODIC ACTIVITY OF RIDGES 174 DIAPIRISM AND
SEGMENTATION 174 THE DIAPIRS: TUBES OR BLOBS? 177 9 THE MAJOR PULSATIONS
OF THE EARTH 179 A GEOLOGICAL POLICE INVESTIGATION 179 A SUPERCONTINENT
AT THE DAWN OF THE MESOZOIC 180 AND TOMORROW? 185 THE PANGEAN CYCLE 186
OPHIOLITES CREATED AT SPRINGTIME 189 GLOSSARY 191 SOURCE OF
ILLUSTRATIONS 199 XVII CONTENTS |
| any_adam_object | 1 |
| author | Nicolas, Adolphe 1936-2020 |
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| bvnumber | BV010013528 |
| callnumber-first | Q - Science |
| callnumber-label | QE511 |
| callnumber-raw | QE511.7 |
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| callnumber-subject | QE - Geology |
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| dewey-full | 551.1/36 |
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| dewey-ones | 551 - Geology, hydrology, meteorology |
| dewey-raw | 551.1/36 |
| dewey-search | 551.1/36 |
| dewey-sort | 3551.1 236 |
| dewey-tens | 550 - Earth sciences |
| discipline | Geowissenschaften Geologie / Paläontologie Geographie |
| format | Book |
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| id | DE-604.BV010013528 |
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| indexdate | 2024-07-20T07:51:09Z |
| institution | BVB |
| isbn | 3540573801 0387573801 |
| language | German English French |
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| physical | XVII, 200 S. Ill., graph. Darst., Kt. |
| publishDate | 1995 |
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| spelling | Nicolas, Adolphe 1936-2020 Verfasser (DE-588)1089202954 aut Les montagnes sous la mer The mid-oceanic ridges mountains below sea level Adolphe Nicolas. [Transl.: Thomas Reimer] Berlin [u.a.] Springer 1995 XVII, 200 S. Ill., graph. Darst., Kt. txt rdacontent n rdamedia nc rdacarrier Dt. Ausg. u.d.T.: Nicolas, Adolphe: Die ozeanischen Rücken Despite turbulent actions of plate tectonics, continents, which since the first cooling of the planet float on its substratum, are a geological record of the history of Earth. Since the existing oceans are geologically relatively young, they register the activity, the life of the Earth. They formed when a large supercontinent (Pangea) broke apart some 150 Ma ago. The mid-oceanic ridges are narrow belts of submarine mountains marking the boundaries between plates which are moving apart, with new oceanic crust being created at the same time. Under the continents oceanic crust is subducted. The ocean bottom is an ideal location to study recent geodynamic processes on Earth. Of special interest to the reader will be the combination of the most recent oceanographic data with ophiolites, representing fossil ocean crust, obducted onto the continents by tectonic processes. Geomorfologia marinha larpcal Mid-ocean ridges Sea-floor spreading Plattentektonik (DE-588)4046317-5 gnd rswk-swf Magmatisches Gestein (DE-588)4036974-2 gnd rswk-swf Ozeanischer Rücken (DE-588)4368695-3 gnd rswk-swf Mittelozeanischer Rücken (DE-588)4317501-6 gnd rswk-swf Ozeanischer Rücken (DE-588)4368695-3 s DE-604 Plattentektonik (DE-588)4046317-5 s Mittelozeanischer Rücken (DE-588)4317501-6 g Magmatisches Gestein (DE-588)4036974-2 s GBV Datenaustausch application/pdf http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=006640036&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA Inhaltsverzeichnis |
| spellingShingle | Nicolas, Adolphe 1936-2020 The mid-oceanic ridges mountains below sea level Geomorfologia marinha larpcal Mid-ocean ridges Sea-floor spreading Plattentektonik (DE-588)4046317-5 gnd Magmatisches Gestein (DE-588)4036974-2 gnd Ozeanischer Rücken (DE-588)4368695-3 gnd |
| subject_GND | (DE-588)4046317-5 (DE-588)4036974-2 (DE-588)4368695-3 (DE-588)4317501-6 |
| title | The mid-oceanic ridges mountains below sea level |
| title_alt | Les montagnes sous la mer |
| 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 Adolphe Nicolas. [Transl.: Thomas Reimer] |
| title_fullStr | The mid-oceanic ridges mountains below sea level Adolphe Nicolas. [Transl.: Thomas Reimer] |
| title_full_unstemmed | The mid-oceanic ridges mountains below sea level Adolphe Nicolas. [Transl.: Thomas Reimer] |
| title_short | The mid-oceanic ridges |
| title_sort | the mid oceanic ridges mountains below sea level |
| title_sub | mountains below sea level |
| topic | Geomorfologia marinha larpcal Mid-ocean ridges Sea-floor spreading Plattentektonik (DE-588)4046317-5 gnd Magmatisches Gestein (DE-588)4036974-2 gnd Ozeanischer Rücken (DE-588)4368695-3 gnd |
| topic_facet | Geomorfologia marinha Mid-ocean ridges Sea-floor spreading Plattentektonik Magmatisches Gestein Ozeanischer Rücken Mittelozeanischer Rücken |
| url | http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=006640036&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA |
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