Oceanic subcrustal flow toward the continents and constancy of global sea-level
Summary From the conservation of the mass of the earth including the hydrosphere it can be concluded that continental growth has been connected with subcrustal flow from the ocean toward the continents. Calculations show that the volume of ocean bottom subsidence nearly equals to the volume of the u...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Boldizsár, T. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1969 |
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| Schlagwörter: |
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| Anmerkung: |
© Birkhäuser-Verlag 1969 |
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| Übergeordnetes Werk: |
Enthalten in: Pure and applied geophysics - Birkhäuser-Verlag, 1964, 72(1969), 1 vom: Dez., Seite 117-122 |
|---|---|
| Übergeordnetes Werk: |
volume:72 ; year:1969 ; number:1 ; month:12 ; pages:117-122 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF00875698 |
|---|
| Katalog-ID: |
OLC206944693X |
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| 520 | |a Summary From the conservation of the mass of the earth including the hydrosphere it can be concluded that continental growth has been connected with subcrustal flow from the ocean toward the continents. Calculations show that the volume of ocean bottom subsidence nearly equals to the volume of the uplifted continental masses above the level of the primeval ocean bottom. The sea level has not changed appreciably since Precambrian. Change of ocean bottom topography and emergence of continents do not effect global sea level. Transgression and regression are figurative terms and really indicate subsidence resp. uplift of the continental crust blocks around the shoreline. | ||
| 650 | 4 | |a Continental Crust | |
| 650 | 4 | |a Bottom Topography | |
| 650 | 4 | |a Ocean Bottom | |
| 650 | 4 | |a Crust Block | |
| 650 | 4 | |a Continental Growth | |
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10.1007/BF00875698 doi (DE-627)OLC206944693X (DE-He213)BF00875698-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Boldizsár, T. verfasserin aut Oceanic subcrustal flow toward the continents and constancy of global sea-level 1969 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1969 Summary From the conservation of the mass of the earth including the hydrosphere it can be concluded that continental growth has been connected with subcrustal flow from the ocean toward the continents. Calculations show that the volume of ocean bottom subsidence nearly equals to the volume of the uplifted continental masses above the level of the primeval ocean bottom. The sea level has not changed appreciably since Precambrian. Change of ocean bottom topography and emergence of continents do not effect global sea level. Transgression and regression are figurative terms and really indicate subsidence resp. uplift of the continental crust blocks around the shoreline. Continental Crust Bottom Topography Ocean Bottom Crust Block Continental Growth Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 72(1969), 1 vom: Dez., Seite 117-122 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:72 year:1969 number:1 month:12 pages:117-122 https://doi.org/10.1007/BF00875698 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_201 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 72 1969 1 12 117-122 |
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10.1007/BF00875698 doi (DE-627)OLC206944693X (DE-He213)BF00875698-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Boldizsár, T. verfasserin aut Oceanic subcrustal flow toward the continents and constancy of global sea-level 1969 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1969 Summary From the conservation of the mass of the earth including the hydrosphere it can be concluded that continental growth has been connected with subcrustal flow from the ocean toward the continents. Calculations show that the volume of ocean bottom subsidence nearly equals to the volume of the uplifted continental masses above the level of the primeval ocean bottom. The sea level has not changed appreciably since Precambrian. Change of ocean bottom topography and emergence of continents do not effect global sea level. Transgression and regression are figurative terms and really indicate subsidence resp. uplift of the continental crust blocks around the shoreline. Continental Crust Bottom Topography Ocean Bottom Crust Block Continental Growth Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 72(1969), 1 vom: Dez., Seite 117-122 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:72 year:1969 number:1 month:12 pages:117-122 https://doi.org/10.1007/BF00875698 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_201 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 72 1969 1 12 117-122 |
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10.1007/BF00875698 doi (DE-627)OLC206944693X (DE-He213)BF00875698-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Boldizsár, T. verfasserin aut Oceanic subcrustal flow toward the continents and constancy of global sea-level 1969 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1969 Summary From the conservation of the mass of the earth including the hydrosphere it can be concluded that continental growth has been connected with subcrustal flow from the ocean toward the continents. Calculations show that the volume of ocean bottom subsidence nearly equals to the volume of the uplifted continental masses above the level of the primeval ocean bottom. The sea level has not changed appreciably since Precambrian. Change of ocean bottom topography and emergence of continents do not effect global sea level. Transgression and regression are figurative terms and really indicate subsidence resp. uplift of the continental crust blocks around the shoreline. Continental Crust Bottom Topography Ocean Bottom Crust Block Continental Growth Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 72(1969), 1 vom: Dez., Seite 117-122 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:72 year:1969 number:1 month:12 pages:117-122 https://doi.org/10.1007/BF00875698 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_201 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 72 1969 1 12 117-122 |
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10.1007/BF00875698 doi (DE-627)OLC206944693X (DE-He213)BF00875698-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Boldizsár, T. verfasserin aut Oceanic subcrustal flow toward the continents and constancy of global sea-level 1969 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1969 Summary From the conservation of the mass of the earth including the hydrosphere it can be concluded that continental growth has been connected with subcrustal flow from the ocean toward the continents. Calculations show that the volume of ocean bottom subsidence nearly equals to the volume of the uplifted continental masses above the level of the primeval ocean bottom. The sea level has not changed appreciably since Precambrian. Change of ocean bottom topography and emergence of continents do not effect global sea level. Transgression and regression are figurative terms and really indicate subsidence resp. uplift of the continental crust blocks around the shoreline. Continental Crust Bottom Topography Ocean Bottom Crust Block Continental Growth Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 72(1969), 1 vom: Dez., Seite 117-122 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:72 year:1969 number:1 month:12 pages:117-122 https://doi.org/10.1007/BF00875698 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_201 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 72 1969 1 12 117-122 |
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10.1007/BF00875698 doi (DE-627)OLC206944693X (DE-He213)BF00875698-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Boldizsár, T. verfasserin aut Oceanic subcrustal flow toward the continents and constancy of global sea-level 1969 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1969 Summary From the conservation of the mass of the earth including the hydrosphere it can be concluded that continental growth has been connected with subcrustal flow from the ocean toward the continents. Calculations show that the volume of ocean bottom subsidence nearly equals to the volume of the uplifted continental masses above the level of the primeval ocean bottom. The sea level has not changed appreciably since Precambrian. Change of ocean bottom topography and emergence of continents do not effect global sea level. Transgression and regression are figurative terms and really indicate subsidence resp. uplift of the continental crust blocks around the shoreline. Continental Crust Bottom Topography Ocean Bottom Crust Block Continental Growth Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 72(1969), 1 vom: Dez., Seite 117-122 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:72 year:1969 number:1 month:12 pages:117-122 https://doi.org/10.1007/BF00875698 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_201 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 72 1969 1 12 117-122 |
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Oceanic subcrustal flow toward the continents and constancy of global sea-level |
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| title_full |
Oceanic subcrustal flow toward the continents and constancy of global sea-level |
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Boldizsár, T. |
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Pure and applied geophysics |
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Pure and applied geophysics |
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1969 |
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117 |
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Boldizsár, T. |
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72 |
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Aufsätze |
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Boldizsár, T. |
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10.1007/BF00875698 |
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550 |
| title_sort |
oceanic subcrustal flow toward the continents and constancy of global sea-level |
| title_auth |
Oceanic subcrustal flow toward the continents and constancy of global sea-level |
| abstract |
Summary From the conservation of the mass of the earth including the hydrosphere it can be concluded that continental growth has been connected with subcrustal flow from the ocean toward the continents. Calculations show that the volume of ocean bottom subsidence nearly equals to the volume of the uplifted continental masses above the level of the primeval ocean bottom. The sea level has not changed appreciably since Precambrian. Change of ocean bottom topography and emergence of continents do not effect global sea level. Transgression and regression are figurative terms and really indicate subsidence resp. uplift of the continental crust blocks around the shoreline. © Birkhäuser-Verlag 1969 |
| abstractGer |
Summary From the conservation of the mass of the earth including the hydrosphere it can be concluded that continental growth has been connected with subcrustal flow from the ocean toward the continents. Calculations show that the volume of ocean bottom subsidence nearly equals to the volume of the uplifted continental masses above the level of the primeval ocean bottom. The sea level has not changed appreciably since Precambrian. Change of ocean bottom topography and emergence of continents do not effect global sea level. Transgression and regression are figurative terms and really indicate subsidence resp. uplift of the continental crust blocks around the shoreline. © Birkhäuser-Verlag 1969 |
| abstract_unstemmed |
Summary From the conservation of the mass of the earth including the hydrosphere it can be concluded that continental growth has been connected with subcrustal flow from the ocean toward the continents. Calculations show that the volume of ocean bottom subsidence nearly equals to the volume of the uplifted continental masses above the level of the primeval ocean bottom. The sea level has not changed appreciably since Precambrian. Change of ocean bottom topography and emergence of continents do not effect global sea level. Transgression and regression are figurative terms and really indicate subsidence resp. uplift of the continental crust blocks around the shoreline. © Birkhäuser-Verlag 1969 |
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Oceanic subcrustal flow toward the continents and constancy of global sea-level |
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