Evolution of the oceanic and continental crust during Neo-Proterozoic and Phanerozoic
Abstract In present, contribution paleogeographical maps for the time interval 0.6 Ga BP to present are analyzed in terms of (a) the ratio between continental to oceanic crust areas in order to estimate the speed of continental growth and (b) the surface motion of continental plates under the influe...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Varga, Peter [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2014 |
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| Schlagwörter: |
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| Anmerkung: |
© Accademia Nazionale dei Lincei 2014 |
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| Übergeordnetes Werk: |
Enthalten in: Rendiconti lincei - Heidelberg : Springer, 1990, 25(2014), 2 vom: 20. März, Seite 255-263 |
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| Übergeordnetes Werk: |
volume:25 ; year:2014 ; number:2 ; day:20 ; month:03 ; pages:255-263 |
| Links: |
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| DOI / URN: |
10.1007/s12210-014-0298-9 |
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SPR025368540 |
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| 100 | 1 | |a Varga, Peter |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Evolution of the oceanic and continental crust during Neo-Proterozoic and Phanerozoic |
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| 520 | |a Abstract In present, contribution paleogeographical maps for the time interval 0.6 Ga BP to present are analyzed in terms of (a) the ratio between continental to oceanic crust areas in order to estimate the speed of continental growth and (b) the surface motion of continental plates under the influence of global forces of tidal friction and Eötvös force (“pole-fleeing”). It is concluded that the area of the continents during the Phanerozoic was growing and it exhibited a rate ~0.5 $ km^{3} $/year. It is also found that beside the westward-oriented tidal frictional forces the Eötvös force can play also a role in tectonical processes. It is shown that the continental plates on average tend to find a position close to the equator during the whole investigated 600 Ma time interval. | ||
| 650 | 4 | |a Plate tectonic reconstructions |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Phanerozoic |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Motion of continental plates |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Tidal friction |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a “Pole-fleeing” force or Eötvös force |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Krumm, Friedhelm W. |4 aut | |
| 700 | 1 | |a Grafarend, Erik W. |4 aut | |
| 700 | 1 | |a Sneeuw, Nico |4 aut | |
| 700 | 1 | |a Schreider, Anatoly A. |4 aut | |
| 700 | 1 | |a Horváth, Frank |4 aut | |
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10.1007/s12210-014-0298-9 doi (DE-627)SPR025368540 (SPR)s12210-014-0298-9-e DE-627 ger DE-627 rakwb eng Varga, Peter verfasserin aut Evolution of the oceanic and continental crust during Neo-Proterozoic and Phanerozoic 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Accademia Nazionale dei Lincei 2014 Abstract In present, contribution paleogeographical maps for the time interval 0.6 Ga BP to present are analyzed in terms of (a) the ratio between continental to oceanic crust areas in order to estimate the speed of continental growth and (b) the surface motion of continental plates under the influence of global forces of tidal friction and Eötvös force (“pole-fleeing”). It is concluded that the area of the continents during the Phanerozoic was growing and it exhibited a rate ~0.5 $ km^{3} $/year. It is also found that beside the westward-oriented tidal frictional forces the Eötvös force can play also a role in tectonical processes. It is shown that the continental plates on average tend to find a position close to the equator during the whole investigated 600 Ma time interval. Plate tectonic reconstructions (dpeaa)DE-He213 Phanerozoic (dpeaa)DE-He213 Motion of continental plates (dpeaa)DE-He213 Tidal friction (dpeaa)DE-He213 “Pole-fleeing” force or Eötvös force (dpeaa)DE-He213 Krumm, Friedhelm W. aut Grafarend, Erik W. aut Sneeuw, Nico aut Schreider, Anatoly A. aut Horváth, Frank aut Enthalten in Rendiconti lincei Heidelberg : Springer, 1990 25(2014), 2 vom: 20. März, Seite 255-263 (DE-627)385615477 (DE-600)2143014-7 1720-0776 nnns volume:25 year:2014 number:2 day:20 month:03 pages:255-263 https://dx.doi.org/10.1007/s12210-014-0298-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 25 2014 2 20 03 255-263 |
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10.1007/s12210-014-0298-9 doi (DE-627)SPR025368540 (SPR)s12210-014-0298-9-e DE-627 ger DE-627 rakwb eng Varga, Peter verfasserin aut Evolution of the oceanic and continental crust during Neo-Proterozoic and Phanerozoic 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Accademia Nazionale dei Lincei 2014 Abstract In present, contribution paleogeographical maps for the time interval 0.6 Ga BP to present are analyzed in terms of (a) the ratio between continental to oceanic crust areas in order to estimate the speed of continental growth and (b) the surface motion of continental plates under the influence of global forces of tidal friction and Eötvös force (“pole-fleeing”). It is concluded that the area of the continents during the Phanerozoic was growing and it exhibited a rate ~0.5 $ km^{3} $/year. It is also found that beside the westward-oriented tidal frictional forces the Eötvös force can play also a role in tectonical processes. It is shown that the continental plates on average tend to find a position close to the equator during the whole investigated 600 Ma time interval. Plate tectonic reconstructions (dpeaa)DE-He213 Phanerozoic (dpeaa)DE-He213 Motion of continental plates (dpeaa)DE-He213 Tidal friction (dpeaa)DE-He213 “Pole-fleeing” force or Eötvös force (dpeaa)DE-He213 Krumm, Friedhelm W. aut Grafarend, Erik W. aut Sneeuw, Nico aut Schreider, Anatoly A. aut Horváth, Frank aut Enthalten in Rendiconti lincei Heidelberg : Springer, 1990 25(2014), 2 vom: 20. März, Seite 255-263 (DE-627)385615477 (DE-600)2143014-7 1720-0776 nnns volume:25 year:2014 number:2 day:20 month:03 pages:255-263 https://dx.doi.org/10.1007/s12210-014-0298-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 25 2014 2 20 03 255-263 |
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10.1007/s12210-014-0298-9 doi (DE-627)SPR025368540 (SPR)s12210-014-0298-9-e DE-627 ger DE-627 rakwb eng Varga, Peter verfasserin aut Evolution of the oceanic and continental crust during Neo-Proterozoic and Phanerozoic 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Accademia Nazionale dei Lincei 2014 Abstract In present, contribution paleogeographical maps for the time interval 0.6 Ga BP to present are analyzed in terms of (a) the ratio between continental to oceanic crust areas in order to estimate the speed of continental growth and (b) the surface motion of continental plates under the influence of global forces of tidal friction and Eötvös force (“pole-fleeing”). It is concluded that the area of the continents during the Phanerozoic was growing and it exhibited a rate ~0.5 $ km^{3} $/year. It is also found that beside the westward-oriented tidal frictional forces the Eötvös force can play also a role in tectonical processes. It is shown that the continental plates on average tend to find a position close to the equator during the whole investigated 600 Ma time interval. Plate tectonic reconstructions (dpeaa)DE-He213 Phanerozoic (dpeaa)DE-He213 Motion of continental plates (dpeaa)DE-He213 Tidal friction (dpeaa)DE-He213 “Pole-fleeing” force or Eötvös force (dpeaa)DE-He213 Krumm, Friedhelm W. aut Grafarend, Erik W. aut Sneeuw, Nico aut Schreider, Anatoly A. aut Horváth, Frank aut Enthalten in Rendiconti lincei Heidelberg : Springer, 1990 25(2014), 2 vom: 20. März, Seite 255-263 (DE-627)385615477 (DE-600)2143014-7 1720-0776 nnns volume:25 year:2014 number:2 day:20 month:03 pages:255-263 https://dx.doi.org/10.1007/s12210-014-0298-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 25 2014 2 20 03 255-263 |
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10.1007/s12210-014-0298-9 doi (DE-627)SPR025368540 (SPR)s12210-014-0298-9-e DE-627 ger DE-627 rakwb eng Varga, Peter verfasserin aut Evolution of the oceanic and continental crust during Neo-Proterozoic and Phanerozoic 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Accademia Nazionale dei Lincei 2014 Abstract In present, contribution paleogeographical maps for the time interval 0.6 Ga BP to present are analyzed in terms of (a) the ratio between continental to oceanic crust areas in order to estimate the speed of continental growth and (b) the surface motion of continental plates under the influence of global forces of tidal friction and Eötvös force (“pole-fleeing”). It is concluded that the area of the continents during the Phanerozoic was growing and it exhibited a rate ~0.5 $ km^{3} $/year. It is also found that beside the westward-oriented tidal frictional forces the Eötvös force can play also a role in tectonical processes. It is shown that the continental plates on average tend to find a position close to the equator during the whole investigated 600 Ma time interval. Plate tectonic reconstructions (dpeaa)DE-He213 Phanerozoic (dpeaa)DE-He213 Motion of continental plates (dpeaa)DE-He213 Tidal friction (dpeaa)DE-He213 “Pole-fleeing” force or Eötvös force (dpeaa)DE-He213 Krumm, Friedhelm W. aut Grafarend, Erik W. aut Sneeuw, Nico aut Schreider, Anatoly A. aut Horváth, Frank aut Enthalten in Rendiconti lincei Heidelberg : Springer, 1990 25(2014), 2 vom: 20. März, Seite 255-263 (DE-627)385615477 (DE-600)2143014-7 1720-0776 nnns volume:25 year:2014 number:2 day:20 month:03 pages:255-263 https://dx.doi.org/10.1007/s12210-014-0298-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 25 2014 2 20 03 255-263 |
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10.1007/s12210-014-0298-9 doi (DE-627)SPR025368540 (SPR)s12210-014-0298-9-e DE-627 ger DE-627 rakwb eng Varga, Peter verfasserin aut Evolution of the oceanic and continental crust during Neo-Proterozoic and Phanerozoic 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Accademia Nazionale dei Lincei 2014 Abstract In present, contribution paleogeographical maps for the time interval 0.6 Ga BP to present are analyzed in terms of (a) the ratio between continental to oceanic crust areas in order to estimate the speed of continental growth and (b) the surface motion of continental plates under the influence of global forces of tidal friction and Eötvös force (“pole-fleeing”). It is concluded that the area of the continents during the Phanerozoic was growing and it exhibited a rate ~0.5 $ km^{3} $/year. It is also found that beside the westward-oriented tidal frictional forces the Eötvös force can play also a role in tectonical processes. It is shown that the continental plates on average tend to find a position close to the equator during the whole investigated 600 Ma time interval. Plate tectonic reconstructions (dpeaa)DE-He213 Phanerozoic (dpeaa)DE-He213 Motion of continental plates (dpeaa)DE-He213 Tidal friction (dpeaa)DE-He213 “Pole-fleeing” force or Eötvös force (dpeaa)DE-He213 Krumm, Friedhelm W. aut Grafarend, Erik W. aut Sneeuw, Nico aut Schreider, Anatoly A. aut Horváth, Frank aut Enthalten in Rendiconti lincei Heidelberg : Springer, 1990 25(2014), 2 vom: 20. März, Seite 255-263 (DE-627)385615477 (DE-600)2143014-7 1720-0776 nnns volume:25 year:2014 number:2 day:20 month:03 pages:255-263 https://dx.doi.org/10.1007/s12210-014-0298-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 25 2014 2 20 03 255-263 |
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Varga, Peter @@aut@@ Krumm, Friedhelm W. @@aut@@ Grafarend, Erik W. @@aut@@ Sneeuw, Nico @@aut@@ Schreider, Anatoly A. @@aut@@ Horváth, Frank @@aut@@ |
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| author |
Varga, Peter |
| spellingShingle |
Varga, Peter misc Plate tectonic reconstructions misc Phanerozoic misc Motion of continental plates misc Tidal friction misc “Pole-fleeing” force or Eötvös force Evolution of the oceanic and continental crust during Neo-Proterozoic and Phanerozoic |
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| topic_title |
Evolution of the oceanic and continental crust during Neo-Proterozoic and Phanerozoic Plate tectonic reconstructions (dpeaa)DE-He213 Phanerozoic (dpeaa)DE-He213 Motion of continental plates (dpeaa)DE-He213 Tidal friction (dpeaa)DE-He213 “Pole-fleeing” force or Eötvös force (dpeaa)DE-He213 |
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misc Plate tectonic reconstructions misc Phanerozoic misc Motion of continental plates misc Tidal friction misc “Pole-fleeing” force or Eötvös force |
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misc Plate tectonic reconstructions misc Phanerozoic misc Motion of continental plates misc Tidal friction misc “Pole-fleeing” force or Eötvös force |
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misc Plate tectonic reconstructions misc Phanerozoic misc Motion of continental plates misc Tidal friction misc “Pole-fleeing” force or Eötvös force |
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Evolution of the oceanic and continental crust during Neo-Proterozoic and Phanerozoic |
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Evolution of the oceanic and continental crust during Neo-Proterozoic and Phanerozoic |
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Varga, Peter |
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Varga, Peter Krumm, Friedhelm W. Grafarend, Erik W. Sneeuw, Nico Schreider, Anatoly A. Horváth, Frank |
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Varga, Peter |
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10.1007/s12210-014-0298-9 |
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evolution of the oceanic and continental crust during neo-proterozoic and phanerozoic |
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Evolution of the oceanic and continental crust during Neo-Proterozoic and Phanerozoic |
| abstract |
Abstract In present, contribution paleogeographical maps for the time interval 0.6 Ga BP to present are analyzed in terms of (a) the ratio between continental to oceanic crust areas in order to estimate the speed of continental growth and (b) the surface motion of continental plates under the influence of global forces of tidal friction and Eötvös force (“pole-fleeing”). It is concluded that the area of the continents during the Phanerozoic was growing and it exhibited a rate ~0.5 $ km^{3} $/year. It is also found that beside the westward-oriented tidal frictional forces the Eötvös force can play also a role in tectonical processes. It is shown that the continental plates on average tend to find a position close to the equator during the whole investigated 600 Ma time interval. © Accademia Nazionale dei Lincei 2014 |
| abstractGer |
Abstract In present, contribution paleogeographical maps for the time interval 0.6 Ga BP to present are analyzed in terms of (a) the ratio between continental to oceanic crust areas in order to estimate the speed of continental growth and (b) the surface motion of continental plates under the influence of global forces of tidal friction and Eötvös force (“pole-fleeing”). It is concluded that the area of the continents during the Phanerozoic was growing and it exhibited a rate ~0.5 $ km^{3} $/year. It is also found that beside the westward-oriented tidal frictional forces the Eötvös force can play also a role in tectonical processes. It is shown that the continental plates on average tend to find a position close to the equator during the whole investigated 600 Ma time interval. © Accademia Nazionale dei Lincei 2014 |
| abstract_unstemmed |
Abstract In present, contribution paleogeographical maps for the time interval 0.6 Ga BP to present are analyzed in terms of (a) the ratio between continental to oceanic crust areas in order to estimate the speed of continental growth and (b) the surface motion of continental plates under the influence of global forces of tidal friction and Eötvös force (“pole-fleeing”). It is concluded that the area of the continents during the Phanerozoic was growing and it exhibited a rate ~0.5 $ km^{3} $/year. It is also found that beside the westward-oriented tidal frictional forces the Eötvös force can play also a role in tectonical processes. It is shown that the continental plates on average tend to find a position close to the equator during the whole investigated 600 Ma time interval. © Accademia Nazionale dei Lincei 2014 |
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Evolution of the oceanic and continental crust during Neo-Proterozoic and Phanerozoic |
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Krumm, Friedhelm W. Grafarend, Erik W. Sneeuw, Nico Schreider, Anatoly A. Horváth, Frank |
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Krumm, Friedhelm W. Grafarend, Erik W. Sneeuw, Nico Schreider, Anatoly A. Horváth, Frank |
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10.1007/s12210-014-0298-9 |
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2024-07-03T15:34:49.479Z |
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|
| score |
7.399393 |