Pacifičko-Antarktički greben — разлика између измена

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Верзија на датум 17. јул 2023. у 03:07

Pacifičko-Antarktički greben (PAR) divergentna je granica tektonske ploče^[1]^[2]^[3] locirana na morskom dnu južnog Tihog okeana, koja razdvaja Tihookeansku ploču od Antarktičke ploče. U nekim vidovima upotrebe on se smatra južnim delom Istočnopacifičkog grebena, uglavnom južno od Čelindžerske zone preloma^[4] i proteže se do Makvorskog trojnog čvora^[5]^[6]^[7] južno od Novog Zelanda.^[8]

Luisvilski greben

Prostire se na 4.300 km sever-zapad od Pacifičko-Antarktičkog grebena do podmorske planine Osborn na spoju Tonga i Kermadeka.^[9] To je dugačak niz podmorskih planina zvanih Luisvilski greben, koji je najduži takav lanac na Tihom okeanu,^[10] i za koji se misli da je nastao od Tihookeanske ploče koja je nadišla preko dugovečnog centra rastopljene magme zvanog žarište Luisvil.

Reference

^ Langmuir, Charles H.; Klein, Emily M.; Plank, Terry (2013). „Petrological Systematics of Mid-Ocean Ridge Basalts: Constraints on Melt Generation Beneath Ocean Ridges”. Mantle Flow and Melt Generation at Mid-Ocean Ridges. Geophysical Monograph Series. стр. 183—280. ISBN 9781118663875. doi:10.1029/GM071p0183. hdl:10161/8316.
^ Sinton, John M.; Detrick, Robert S. (1992). „Mid-ocean ridge magma chambers”. Journal of Geophysical Research. 97 (B1): 197. Bibcode:1992JGR....97..197S. doi:10.1029/91JB02508.
^ Toshiro Tanimoto; Thorne Lay (7. 11. 2000). „Mantle dynamics and seismic tomography”. Proc. Natl. Acad. Sci. U.S.A. 97 (23): 12409—10. Bibcode:2000PNAS...9712409T. PMC 34063 . PMID 11035784. doi:10.1073/pnas.210382197 .
^ Yáñez, G.; Cembrano, J.; Pardo, M.; Ranero, C.; Selles, D. (2002). „The Challenger–Juan Fernández–Maipo major tectonic transition of the Nazca–Andean subduction system at 33–34°S: geodynamic evidence and implications”. стр. 23—38. doi:10.1016/S0895-9811(02)00004-4.
^ Marks (1997). „Early Tertiary gravity field reconstructions of the Southwest pacific.”. Earth and Planetary Science Letters: 152: 267—274.
^ Meckel (2003). Tectonics of the Hjort region of the Macquarie Ridge Complex, southernmost Australian-Pacific Plate Boundary, southwest Pacific Ocean (PhD) (Теза). стр. 206. Bibcode:2003PhDT.......206M.
^ Harbert W.; Cox A. (1989). „Late Neogene motion of the Pacific Plate”. Journal of Geophysical Research. 94: 3052—3064.
^ „Pacific-Antarctic Ridge”. www.britannica.com. Приступљено 5. 4. 2013.
^ Keating, Barbara H. (1987). Seamounts, Islands, and Atolls. American Geophysical Union. ISBN 0-87590-068-2.
^ Q. Cheng; K.H. Park; J. D. Macdougall; A. Zindler; G. W. Lugmair; H. Staudigel; J. Hawkins; P. Lonsdale (1987). Barbara H. Keating; Patricia Fryer; Rodey Batiza; George W. Boehlert, ур. „Isotopic Evidence for a Hotspot Origin of the Louisville Seamount Chain”. Geophysical Monograph Series. doi:10.1029/GM043p0283. Приступљено 2023-07-16.

Literatura

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Koppers, Anthony A. P.; Yamazaki, Toshitsugu; Geldmacher, Jörg; Gee, Jeffrey S.; Pressling, Nicola; Koppers, Anthony A. P.; Yamazaki, Toshitsugu; Geldmacher, Jörg; Gee, Jeffrey S.; Pressling, Nicola; Hoshi, Hiroyuki (децембар 2012). „Limited latitudinal mantle plume motion for the Louisville hotspot”. Nature Geoscience (на језику: енглески). 5 (12): 911—917. Bibcode:2012NatGe...5..911K. ISSN 1752-0908. doi:10.1038/ngeo1638.
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Spoljašnje veze

Morgan, W. Jason; Morgan, Jason Phipps (2007). „Plate velocities in hotspot reference frame: electronic supplement” (PDF). geosociety.org. стр. 55—57.
„What is the longest mountain range on earth?”. Ocean Facts. NOAA. Приступљено 17. 10. 2014.
„Marine Gazetteer Placedetails”. Приступљено 2017-02-20.
Sandwell, David T.; Walter H.F. Smith (1997). „Exploring the ocean basins with satellite altimeter data”. Satellite Geodesy. La Jolla: Scripps Institution of Oceanography. Приступљено 2010-01-19. „The Louisville Ridge was first detected in 1972 using depth soundings collected along random ship crossings of the South Pacific. Six years later the full extent of this chain was revealed by a radar altimeter aboard the Seasat (NASA) spacecraft.”

61° 59′ 58″ Ј; 157° 00′ 01″ З / 61.999555° Ј; 157.000165° З

[1] Langmuir, Charles H.; Klein, Emily M.; Plank, Terry (2013). „Petrological Systematics of Mid-Ocean Ridge Basalts: Constraints on Melt Generation Beneath Ocean Ridges”. Mantle Flow and Melt Generation at Mid-Ocean Ridges. Geophysical Monograph Series. стр. 183—280. ISBN 9781118663875. doi:10.1029/GM071p0183. hdl:10161/8316.

[2] Sinton, John M.; Detrick, Robert S. (1992). „Mid-ocean ridge magma chambers”. Journal of Geophysical Research. 97 (B1): 197. Bibcode:1992JGR....97..197S. doi:10.1029/91JB02508.

[3] Toshiro Tanimoto; Thorne Lay (7. 11. 2000). „Mantle dynamics and seismic tomography”. Proc. Natl. Acad. Sci. U.S.A. 97 (23): 12409—10. Bibcode:2000PNAS...9712409T. PMC 34063 . PMID 11035784. doi:10.1073/pnas.210382197 .

[4] Yáñez, G.; Cembrano, J.; Pardo, M.; Ranero, C.; Selles, D. (2002). „The Challenger–Juan Fernández–Maipo major tectonic transition of the Nazca–Andean subduction system at 33–34°S: geodynamic evidence and implications”. стр. 23—38. doi:10.1016/S0895-9811(02)00004-4.

[5] Marks (1997). „Early Tertiary gravity field reconstructions of the Southwest pacific.”. Earth and Planetary Science Letters: 152: 267—274.

[Meckel-6] Meckel (2003). Tectonics of the Hjort region of the Macquarie Ridge Complex, southernmost Australian-Pacific Plate Boundary, southwest Pacific Ocean (PhD) (Теза). стр. 206. Bibcode:2003PhDT.......206M.

[Harbert-7] Harbert W.; Cox A. (1989). „Late Neogene motion of the Pacific Plate”. Journal of Geophysical Research. 94: 3052—3064.

[brit-8] „Pacific-Antarctic Ridge”. www.britannica.com. Приступљено 5. 4. 2013.

[keat-9] Keating, Barbara H. (1987). Seamounts, Islands, and Atolls. American Geophysical Union. ISBN 0-87590-068-2.

[agu-10] Q. Cheng; K.H. Park; J. D. Macdougall; A. Zindler; G. W. Lugmair; H. Staudigel; J. Hawkins; P. Lonsdale (1987). Barbara H. Keating; Patricia Fryer; Rodey Batiza; George W. Boehlert, ур. „Isotopic Evidence for a Hotspot Origin of the Louisville Seamount Chain”. Geophysical Monograph Series. doi:10.1029/GM043p0283. Приступљено 2023-07-16.

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@@ Ред 1: / Ред 1: @@
 {{short description|Granica tektonske ploče u južnom Tihom okeanu}}
-[[Image:East Pacific Rise.jpg|thumb|300px|Pacifičko-Antarktički greben je južna ekstenzija [[Istočnopacifički greben|Istočnopacifičkog grebena]].]]
+[[Image:East Pacific Rise.jpg|thumb|250px|Pacifičko-Antarktički greben je južna ekstenzija [[Istočnopacifički greben|Istočnopacifičkog grebena]].]]
-'''Pacifičko-Antarktički greben (PAR)''' divergentna je granica [[tectonics|tektonske]] ploče locirana na morskom dnu južnog [[Pacific Ocean|Tihog okeana]], koja razdvaja [[Тихоокеанска плоча|Tihookeansku ploču]] od [[Antarctic Plate|Antarktičke ploče]]. U nekim vidovima upotrebe on se smatra južnim delom [[Istočnopacifički greben|Istočnopacifičkog grebena]], uglavnom južno od [[Challenger Fracture Zone|Čelindžerske zone preloma]] i proteže se do [[Macquarie Triple Junction|Makvorskog trojnog čvora]] južno od [[New Zealand|Novog Zelanda]].<ref name="brit">{{cite web|title=Pacific-Antarctic Ridge|url=http://www.britannica.com/EBchecked/topic/437577/Pacific-Antarctic-Ridge|publisher=www.britannica.com|accessdate=5 April 2013}}</ref>
+'''Pacifičko-Antarktički greben (PAR)''' divergentna je granica [[tectonics|tektonske]] ploče<ref>{{Cite book | doi=10.1029/GM071p0183| chapter=Petrological Systematics of Mid-Ocean Ridge Basalts: Constraints on Melt Generation Beneath Ocean Ridges| title=Mantle Flow and Melt Generation at Mid-Ocean Ridges| pages=183–280| series=Geophysical Monograph Series| year=2013| last1=Langmuir| first1=Charles H.| last2=Klein| first2=Emily M.| last3=Plank| first3=Terry| isbn=9781118663875| hdl=10161/8316}}</ref><ref>{{Cite journal |doi = 10.1029/91JB02508|title = Mid-ocean ridge magma chambers|journal = Journal of Geophysical Research|volume = 97|issue = B1|pages = 197|year = 1992|last1 = Sinton|first1 = John M.|last2 = Detrick|first2 = Robert S.|bibcode = 1992JGR....97..197S}}</ref><ref>{{cite journal | author1 = Toshiro Tanimoto |author2= Thorne Lay |authorlink2=Thorne Lay| date = November 7, 2000 | title = Mantle dynamics and seismic tomography | journal =Proc. Natl. Acad. Sci. U.S.A. | volume =97 | issue =23 | pages = 12409–10 | doi = 10.1073/pnas.210382197 | pmid = 11035784 | pmc = 34063 | bibcode=2000PNAS...9712409T|doi-access= free }}</ref> locirana na morskom dnu južnog [[Pacific Ocean|Tihog okeana]], koja razdvaja [[Тихоокеанска плоча|Tihookeansku ploču]] od [[Antarctic Plate|Antarktičke ploče]]. U nekim vidovima upotrebe on se smatra južnim delom [[Istočnopacifički greben|Istočnopacifičkog grebena]], uglavnom južno od [[Challenger Fracture Zone|Čelindžerske zone preloma]]<ref>{{cite web |url = Journal of South American Earth Sciences |volume = 15 |issue = 1 |date = 2002 |pages = 23-38 |title = The Challenger–Juan Fernández–Maipo major tectonic transition of the Nazca–Andean subduction system at 33–34°S: geodynamic evidence and implications |doi = 10.1016/S0895-9811(02)00004-4 |url = https://www.sciencedirect.com/science/article/abs/pii/S0895981102000044 |author =  Yáñez, G. |author2 = Cembrano, J. |author3 = Pardo, M. |author4 = Ranero, C. |author5 = Selles, D. }}</ref> i proteže se do [[Macquarie Triple Junction|Makvorskog trojnog čvora]]<ref>{{cite journal|last1=Marks|title=Early Tertiary gravity field reconstructions of the Southwest pacific.|date=1997|journal=Earth and Planetary Science Letters|pages=152: 267–274}}</ref><ref name=Meckel>{{cite thesis|last1=Meckel|title=Tectonics of the Hjort region of the Macquarie Ridge Complex, southernmost Australian-Pacific Plate Boundary, southwest Pacific Ocean (PhD)|pages=206|date=2003|bibcode=2003PhDT.......206M}}</ref><ref name=Harbert>{{cite journal|author1=Harbert W.  |author2=Cox A.|title=Late Neogene motion of the Pacific Plate|date=1989|volume=94|journal=Journal of Geophysical Research|pages=3052–3064}}</ref> južno od [[New Zealand|Novog Zelanda]].<ref name="brit">{{cite web|title=Pacific-Antarctic Ridge|url=http://www.britannica.com/EBchecked/topic/437577/Pacific-Antarctic-Ridge|publisher=www.britannica.com|accessdate=5 April 2013}}</ref>
 == Luisvilski greben ==
 [[File:Louisville seamount chain - bathymetry.jpg|thumb|250px|[[Louisville Ridge|Luisvilski greben]]]]
-Prostire se na 4.300 km sever-zapad od Pacifičko-Antarktičkog grebena do podmorske planine [[Osbourn Seamount|Osborn]] na spoju [[Tonga]] i Kermadeka.<ref name="keat">{{cite book|last=Keating|first=Barbara H.|title=Seamounts, Islands, and Atolls|year=1987|publisher=American Geophysical Union|isbn=0-87590-068-2|url=https://books.google.com/?id=u-NMJaicckMC&pg=PA235&lpg=PA235&dq=Louisville+seamount+chain#v=onepage&q=Louisville%20seamount%20chain&f=false}}{{Мртва веза}}</ref> To je dugačak niz podmorskih planina zvanih [[Louisville Ridge|Luisvilski greben]], koji je najduži takav lanac na Tihom okeanu,<ref name="agu">{{cite web|title=Isotopic evidence for a hotspot origin of the Louisville Seamount Chain|url=http://www.agu.org/books/gm/v043/GM043p0283/GM043p0283.shtml|publisher=www.agu.org|accessdate=5 April 2013}}{{Мртва веза}}</ref> i za koji se misli da je nastao od Tihookeanske ploče koja je nadišla preko dugovečnog centra rastopljene [[magma|magme]] zvanog [[Louisville hotspot|žarište Luisvil]].
+Prostire se na 4.300 km sever-zapad od Pacifičko-Antarktičkog grebena do podmorske planine [[Osbourn Seamount|Osborn]] na spoju [[Tonga]] i Kermadeka.<ref name="keat">{{cite book|last=Keating|first=Barbara H.|title=Seamounts, Islands, and Atolls|year=1987|publisher=American Geophysical Union|isbn=0-87590-068-2 |url= https://agupubs.onlinelibrary.wiley.com/doi/book/10.1029/GM043 }} </ref> To je dugačak niz podmorskih planina zvanih [[Louisville Ridge|Luisvilski greben]], koji je najduži takav lanac na Tihom okeanu,<ref name="agu">{{cite web|title=Isotopic Evidence for a Hotspot Origin of the Louisville Seamount Chain
+|author = Q. Cheng |author2 = K.H. Park |author3 = J. D. Macdougall |author4 =  A. Zindler |author5 =  G. W. Lugmair |author6 =  H. Staudigel |author7 = J. Hawkins |author8 =  P. Lonsdale |url=https://agupubs.onlinelibrary.wiley.com/doi/10.1029/GM043p0283 |accessdate= 2023-07-16 |editor = Barbara H. Keating |editor2 = Patricia Fryer |editor3 = Rodey Batiza |editor4 = George W. Boehlert |date = 1987 |doi = 10.1029/GM043p0283 |series= Geophysical Monograph Series }}</ref> i za koji se misli da je nastao od Tihookeanske ploče koja je nadišla preko dugovečnog centra rastopljene [[magma|magme]] zvanog [[Louisville hotspot|žarište Luisvil]].
 == Reference ==
@@ Ред 28: / Ред 29: @@
 * {{Cite journal|last1=Vine|first1=F. J.|last2=Matthews|first2=D. H.|date=1963|title=Magnetic Anomalies Over Oceanic Ridges|journal=Nature |language=en|volume=199|issue=4897 |pages=947–949|doi=10.1038/199947a0|issn=0028-0836|bibcode=1963Natur.199..947V|s2cid=4296143}}
 * {{Cite journal|last=Vine|first=F. J.|date=1966-12-16|title=Spreading of the Ocean Floor: New Evidence|journal=Science|language=en|volume=154|issue=3755 |pages=1405–1415|doi=10.1126/science.154.3755.1405|pmid=17821553|issn=0036-8075|bibcode=1966Sci...154.1405V|s2cid=44362406}}
-* {{Cite book|title=Mid-ocean ridges|last=Searle, Roger, 1944–|isbn=9781107017528|location=New York|oclc=842323181|date = 2013-09-19}}
+* {{Cite book|title=Mid-ocean ridges | author =Searle, Roger |isbn=9781107017528|location=New York|oclc=842323181|date = 2013-09-19}}
 * {{Cite journal|last=Macdonald|first=Ken C.|date=1977|title=Near-bottom magnetic anomalies, asymmetric spreading, oblique spreading, and tectonics of the Mid-Atlantic Ridge near lat 37°N|url=https://archive.org/details/sim_geological-society-of-america-bulletin_1977-04_88_4/page/541|journal=Geological Society of America Bulletin|language=en|volume=88|issue=4|pages=541|doi=10.1130/0016-7606(1977)88<541:NMAASO>2.0.CO;2|issn=0016-7606|bibcode=1977GSAB...88..541M}}
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@@ Ред 34: / Ред 35: @@
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 {{refend}}