Okinavska ploča: razlika između inačica

Posljednja izmjena od 1. svibanj 2022. u 04:24

{{#invoke:Infobox|infobox}} Okinavska ploča je manja kontinentalna tektonska ploča na sjevernoj i istočnoj polutci koja se proteže od sjevernog kraja Tajvana do južnog rta otoka Kyūshūa.^[1]^[2] Okinavska ploča odgovorna je za potrese, poput potresa na potresa na otoku Kikai 1911., i razne vrste sporih potresa, uključujući potrese niske frekvencije,^[3] potrese vrlo niske frekvencije,^[4] podrhtavanje,^[5] i događaje sporog klizanja.^[6]

Granice[uredi]

Istočna strana Okinavske ploče čini konvergentnu granicu s Filipinskom pločom , tvoreći jarak Ryukyu i otočni luk koji tvori otočje Ryū Kyū. Okinavska ploča je sa zapadne strane omeđena Okinavskim jarkom, zalučnim bazenom i divergentnom granicom s pločom Jangce. Dio južne granice između ploče Okinawa i Filipinske ploče je bivša zona subdukcije koja sada prihvaća koso klizanje i na kojoj se dogodio Velikog tsunami u Yaeyami 1771. godine.^[7]^[8] Sjeverna strana Okinawske ploče omeđena je Amurskom pločom.

Izvori[uredi]

↑ Sibuet, Jean-Claude; Letouzey, Jean; Barbier, Florence; Charvet, Jacques; Foucher, Jean-Paul; Hilde, Thomas W. C.; Kimura, Masaaki; Chiao, Ling-Yun et al. (1987). "Back Arc Extension in the Okinawa Trough" (engl.). Journal of Geophysical Research: Solid Earth 92 (B13): 14041–14063. doi:10.1029/JB092iB13p14041. ISSN 2156-2202 nevaljani ISSN. https://semanticscholar.org/paper/b423e236ca0d17b33248f044f35505d1f1109f3f
↑ Lin, Jing-Yi; Sibuet, Jean-Claude; Lee, Chao-Shing; Hsu, Shu-Kun; Klingelhoefer, Frauke; Auffret, Yves; Pelleau, Pascal; Crozon, Jacques et al. (2009). "Microseismicity and faulting in the southwestern Okinawa Trough". Tectonophysics 466 (3–4): 268–280. doi:10.1016/j.tecto.2007.11.030. ISSN 0040-1951 nevaljani ISSN
↑ Katsumata, Akio; Kamaya, Noriko (2003). "Low-frequency continuous tremor around the Moho discontinuity away from volcanoes in the southwest Japan". Geophysical Research Letters 30 (1): 20–1-20-4. doi:10.1029/2002gl015981. ISSN 0094-8276 nevaljani ISSN. https://semanticscholar.org/paper/9e27d18bc377a34d75c8e66858ead01ba44c3c83
↑ Nakamura, Mamoru; Sunagawa, Naoya (24. veljača 2015.). "Activation of very low frequency earthquakes by slow slip events in the Ryukyu Trench". Geophysical Research Letters 42 (4): 1076–1082. doi:10.1002/2014gl062929. ISSN 0094-8276 nevaljani ISSN
↑ Yamashita, Y.; Yakiwara, H.; Asano, Y.; Shimizu, H.; Uchida, K.; Hirano, S.; Umakoshi, K.; Miyamachi, H. et al. (7. svibanj 2015.). "Migrating tremor off southern Kyushu as evidence for slow slip of a shallow subduction interface". Science 348 (6235): 676–679. doi:10.1126/science.aaa4242. ISSN 0036-8075 nevaljani ISSN. PMID 25954006
↑ Nishimura, Takuya (11. listopad 2014.). "Short-term slow slip events along the Ryukyu Trench, southwestern Japan, observed by continuous GNSS". Progress in Earth and Planetary Science 1 (1). doi:10.1186/s40645-014-0022-5. ISSN 2197-4284 nevaljani ISSN
↑ Bird, Peter (2003). "An updated digital model of plate boundaries: UPDATED MODEL OF PLATE BOUNDARIES" (engl.). Geochemistry, Geophysics, Geosystems 4 (3). doi:10.1029/2001GC000252
↑ Okamura, Yukinobu; Nishizawa, Azusa; Fujii, Yushiro; Yanagisawa, Hideaki (11. rujan 2018.). "Accretionary prism collapse: a new hypothesis on the source of the 1771 giant tsunami in the Ryukyu Arc, SW Japan". Scientific Reports 8 (1): 13620. doi:10.1038/s41598-018-31956-8. ISSN 2045-2322 nevaljani ISSN. PMC 6134009. PMID 30206405. //www.ncbi.nlm.nih.gov/pmc/articles/PMC6134009/

[1] Sibuet, Jean-Claude; Letouzey, Jean; Barbier, Florence; Charvet, Jacques; Foucher, Jean-Paul; Hilde, Thomas W. C.; Kimura, Masaaki; Chiao, Ling-Yun et al. (1987). "Back Arc Extension in the Okinawa Trough" (engl.). Journal of Geophysical Research: Solid Earth 92 (B13): 14041–14063. doi:10.1029/JB092iB13p14041. ISSN 2156-2202 nevaljani ISSN. https://semanticscholar.org/paper/b423e236ca0d17b33248f044f35505d1f1109f3f

[2] Lin, Jing-Yi; Sibuet, Jean-Claude; Lee, Chao-Shing; Hsu, Shu-Kun; Klingelhoefer, Frauke; Auffret, Yves; Pelleau, Pascal; Crozon, Jacques et al. (2009). "Microseismicity and faulting in the southwestern Okinawa Trough". Tectonophysics 466 (3–4): 268–280. doi:10.1016/j.tecto.2007.11.030. ISSN 0040-1951 nevaljani ISSN

[3] Katsumata, Akio; Kamaya, Noriko (2003). "Low-frequency continuous tremor around the Moho discontinuity away from volcanoes in the southwest Japan". Geophysical Research Letters 30 (1): 20–1-20-4. doi:10.1029/2002gl015981. ISSN 0094-8276 nevaljani ISSN. https://semanticscholar.org/paper/9e27d18bc377a34d75c8e66858ead01ba44c3c83

[4] Nakamura, Mamoru; Sunagawa, Naoya (24. veljača 2015.). "Activation of very low frequency earthquakes by slow slip events in the Ryukyu Trench". Geophysical Research Letters 42 (4): 1076–1082. doi:10.1002/2014gl062929. ISSN 0094-8276 nevaljani ISSN

[5] Yamashita, Y.; Yakiwara, H.; Asano, Y.; Shimizu, H.; Uchida, K.; Hirano, S.; Umakoshi, K.; Miyamachi, H. et al. (7. svibanj 2015.). "Migrating tremor off southern Kyushu as evidence for slow slip of a shallow subduction interface". Science 348 (6235): 676–679. doi:10.1126/science.aaa4242. ISSN 0036-8075 nevaljani ISSN. PMID 25954006

[6] Nishimura, Takuya (11. listopad 2014.). "Short-term slow slip events along the Ryukyu Trench, southwestern Japan, observed by continuous GNSS". Progress in Earth and Planetary Science 1 (1). doi:10.1186/s40645-014-0022-5. ISSN 2197-4284 nevaljani ISSN

[7] Bird, Peter (2003). "An updated digital model of plate boundaries: UPDATED MODEL OF PLATE BOUNDARIES" (engl.). Geochemistry, Geophysics, Geosystems 4 (3). doi:10.1029/2001GC000252

[8] Okamura, Yukinobu; Nishizawa, Azusa; Fujii, Yushiro; Yanagisawa, Hideaki (11. rujan 2018.). "Accretionary prism collapse: a new hypothesis on the source of the 1771 giant tsunami in the Ryukyu Arc, SW Japan". Scientific Reports 8 (1): 13620. doi:10.1038/s41598-018-31956-8. ISSN 2045-2322 nevaljani ISSN. PMC 6134009. PMID 30206405. //www.ncbi.nlm.nih.gov/pmc/articles/PMC6134009/

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@@ Redak 1: / Redak 1: @@
 {{Tektonska ploča
 | name = Ploča Okinawa
-| image = File:OkinawaPlate.png
+| image = Datoteka:OkinawaPlate.png
 | alt =
 | type = [[Litosferne ploče#Mikroploče|Mikroploča]]
@@ Redak 9: / Redak 9: @@
 | geo_features = [[Okinawa]], [[Tajvan]]
 | color_on_map = }}
-'''Ploča Okinawa''' je manja kontinentalna [[Tektonika ploča|tektonska ploča]] na [[Sjeverna polutka|sjevernoj]] i [[Istočna polutka|istočnoj]] polutci koja se proteže od sjevernog kraja [[Republika Kina|Tajvana]] do južnog rta otoka [[Kyūshū]].<ref>{{Cite journal|last=Sibuet|first=Jean-Claude|last2=Letouzey|first2=Jean|last3=Barbier|first3=Florence|last4=Charvet|first4=Jacques|last5=Foucher|first5=Jean-Paul|last6=Hilde|first6=Thomas W. C.|last7=Kimura|first7=Masaaki|last8=Chiao|first8=Ling-Yun|last9=Marsset|first9=Bruno|date=1987|title=Back Arc Extension in the Okinawa Trough|journal=Journal of Geophysical Research: Solid Earth|language=en|volume=92|issue=B13|pages=14041–14063|doi=10.1029/JB092iB13p14041|issn=2156-2202|url=https://semanticscholar.org/paper/b423e236ca0d17b33248f044f35505d1f1109f3f}}</ref><ref>{{Cite journal|last=Lin|first=Jing-Yi|last2=Sibuet|first2=Jean-Claude|last3=Lee|first3=Chao-Shing|last4=Hsu|first4=Shu-Kun|last5=Klingelhoefer|first5=Frauke|last6=Auffret|first6=Yves|last7=Pelleau|first7=Pascal|last8=Crozon|first8=Jacques|last9=Lin|first9=Cheng-Horng|date=2009|title=Microseismicity and faulting in the southwestern Okinawa Trough |journal=Tectonophysics|volume=466|issue=3–4|pages=268–280|doi=10.1016/j.tecto.2007.11.030|issn=0040-1951}}</ref> Ploča Okinawa odgovorna je za [[potres]]e, poput potresa na [[Potres na otoku Kikai 1911|potresa na otoku Kikai 1911.]], i razne vrste [[Spori potres|sporih potresa]], uključujući potrese niske frekvencije,<ref>{{Cite journal|last=Katsumata|first=Akio|last2=Kamaya|first2=Noriko|date=2003|title=Low-frequency continuous tremor around the Moho discontinuity away from volcanoes in the southwest Japan |journal=Geophysical Research Letters|volume=30|issue=1|pages=20–1-20-4|doi=10.1029/2002gl015981|issn=0094-8276|url=https://semanticscholar.org/paper/9e27d18bc377a34d75c8e66858ead01ba44c3c83}}</ref> potrese vrlo niske frekvencije,<ref>{{Cite journal|last=Nakamura|first=Mamoru|last2=Sunagawa|first2=Naoya|date=2015-02-24|title=Activation of very low frequency earthquakes by slow slip events in the Ryukyu Trench |journal=Geophysical Research Letters|volume=42|issue=4|pages=1076–1082|doi=10.1002/2014gl062929|issn=0094-8276|doi-access=free}}</ref> podrhtavanje,<ref>{{Cite journal|last=Yamashita|first=Y.|last2=Yakiwara|first2=H.|last3=Asano|first3=Y.|last4=Shimizu|first4=H.|last5=Uchida|first5=K.|last6=Hirano|first6=S.|last7=Umakoshi|first7=K.|last8=Miyamachi|first8=H.|last9=Nakamoto|first9=M.|date=2015-05-07|title=Migrating tremor off southern Kyushu as evidence for slow slip of a shallow subduction interface |journal=Science|volume=348|issue=6235|pages=676–679|doi=10.1126/science.aaa4242|pmid=25954006|issn=0036-8075}}</ref> i događaje sporog klizanja.<ref>{{Cite journal|last=Nishimura|first=Takuya|date=2014-10-11|title=Short-term slow slip events along the Ryukyu Trench, southwestern Japan, observed by continuous GNSS |journal=Progress in Earth and Planetary Science|volume=1|issue=1|doi=10.1186/s40645-014-0022-5|issn=2197-4284|doi-access=free}}</ref>
+'''Okinavska ploča''' je manja kontinentalna [[Tektonika ploča|tektonska ploča]] na [[Sjeverna polutka|sjevernoj]] i [[Istočna polutka|istočnoj]] polutci koja se proteže od sjevernog kraja [[Republika Kina|Tajvana]] do južnog rta otoka [[Kyūshū]]a.<ref>{{Cite journal|last=Sibuet|first=Jean-Claude|last2=Letouzey|first2=Jean|last3=Barbier|first3=Florence|last4=Charvet|first4=Jacques|last5=Foucher|first5=Jean-Paul|last6=Hilde|first6=Thomas W. C.|last7=Kimura|first7=Masaaki|last8=Chiao|first8=Ling-Yun|last9=Marsset|first9=Bruno|date=1987|title=Back Arc Extension in the Okinawa Trough|journal=Journal of Geophysical Research: Solid Earth|language=en|volume=92|issue=B13|pages=14041–14063|doi=10.1029/JB092iB13p14041|issn=2156-2202|url=https://semanticscholar.org/paper/b423e236ca0d17b33248f044f35505d1f1109f3f}}</ref><ref>{{Cite journal|last=Lin|first=Jing-Yi|last2=Sibuet|first2=Jean-Claude|last3=Lee|first3=Chao-Shing|last4=Hsu|first4=Shu-Kun|last5=Klingelhoefer|first5=Frauke|last6=Auffret|first6=Yves|last7=Pelleau|first7=Pascal|last8=Crozon|first8=Jacques|last9=Lin|first9=Cheng-Horng|date=2009|title=Microseismicity and faulting in the southwestern Okinawa Trough |journal=Tectonophysics|volume=466|issue=3–4|pages=268–280|doi=10.1016/j.tecto.2007.11.030|issn=0040-1951}}</ref> Okinavska ploča odgovorna je za [[potres]]e, poput potresa na [[Potres na otoku Kikai 1911|potresa na otoku Kikai 1911.]], i razne vrste [[Spori potres|sporih potresa]], uključujući potrese niske frekvencije,<ref>{{Cite journal|last=Katsumata|first=Akio|last2=Kamaya|first2=Noriko|date=2003|title=Low-frequency continuous tremor around the Moho discontinuity away from volcanoes in the southwest Japan |journal=Geophysical Research Letters|volume=30|issue=1|pages=20–1-20-4|doi=10.1029/2002gl015981|issn=0094-8276|url=https://semanticscholar.org/paper/9e27d18bc377a34d75c8e66858ead01ba44c3c83}}</ref> potrese vrlo niske frekvencije,<ref>{{Cite journal|last=Nakamura|first=Mamoru|last2=Sunagawa|first2=Naoya|date=2015-02-24|title=Activation of very low frequency earthquakes by slow slip events in the Ryukyu Trench |journal=Geophysical Research Letters|volume=42|issue=4|pages=1076–1082|doi=10.1002/2014gl062929|issn=0094-8276|doi-access=free}}</ref> podrhtavanje,<ref>{{Cite journal|last=Yamashita|first=Y.|last2=Yakiwara|first2=H.|last3=Asano|first3=Y.|last4=Shimizu|first4=H.|last5=Uchida|first5=K.|last6=Hirano|first6=S.|last7=Umakoshi|first7=K.|last8=Miyamachi|first8=H.|last9=Nakamoto|first9=M.|date=2015-05-07|title=Migrating tremor off southern Kyushu as evidence for slow slip of a shallow subduction interface |journal=Science|volume=348|issue=6235|pages=676–679|doi=10.1126/science.aaa4242|pmid=25954006|issn=0036-8075}}</ref> i događaje sporog klizanja.<ref>{{Cite journal|last=Nishimura|first=Takuya|date=2014-10-11|title=Short-term slow slip events along the Ryukyu Trench, southwestern Japan, observed by continuous GNSS |journal=Progress in Earth and Planetary Science|volume=1|issue=1|doi=10.1186/s40645-014-0022-5|issn=2197-4284|doi-access=free}}</ref>
 == Granice ==
-Istočna strana ploče Okinawa čini [[Konvergentna granica|konvergentnu granicu]] s [[Filipinska ploča|Filipinskom pločom]] , tvoreći [[jarak Ryukyu]] i [[otočni luk]] koji tvori otočje [[Ryū Kyū]]. Ploča Okinawa je sa zapadne strane omeđena [[Okinavski jarak|Okinavskim jarkom]], [[zalučni bazen|zalučnim bazenom]] i [[Divergentna granica|divergentnom granicom]] s [[Ploča Jangce|pločom Jangce]]. Dio južne granice između ploče Okinawa i Filipinske ploče je bivša [[Subdukcija|zona subdukcije]] koja sada prihvaća [[Rasjed|koso klizanje]] i na kojoj se dogodio [[Velikog tsunami u Yaeyami 1771.]] godine.<ref>{{Cite journal|last=Bird|first=Peter|date=2003|title=An updated digital model of plate boundaries: UPDATED MODEL OF PLATE BOUNDARIES|journal=Geochemistry, Geophysics, Geosystems|language=en|volume=4|issue=3|doi=10.1029/2001GC000252|doi-access=free}}</ref><ref>{{Cite journal|last=Okamura|first=Yukinobu|last2=Nishizawa|first2=Azusa|last3=Fujii|first3=Yushiro|last4=Yanagisawa|first4=Hideaki|date=2018-09-11|title=Accretionary prism collapse: a new hypothesis on the source of the 1771 giant tsunami in the Ryukyu Arc, SW Japan|journal=Scientific Reports|volume=8|issue=1|pages=13620|doi=10.1038/s41598-018-31956-8|pmid=30206405|issn=2045-2322|pmc=6134009}}</ref> Sjeverna strana Okinawske ploče omeđena je [[Amurska ploča|Amurskom pločom]].
+Istočna strana Okinavske ploče čini [[Konvergentna granica|konvergentnu granicu]] s [[Filipinska ploča|Filipinskom pločom]] , tvoreći [[jarak Ryukyu]] i [[otočni luk]] koji tvori otočje [[Ryū Kyū]]. Okinavska ploča je sa zapadne strane omeđena [[Okinavski jarak|Okinavskim jarkom]], [[zalučni bazen|zalučnim bazenom]] i [[Divergentna granica|divergentnom granicom]] s [[Ploča Jangce|pločom Jangce]]. Dio južne granice između ploče Okinawa i Filipinske ploče je bivša [[Subdukcija|zona subdukcije]] koja sada prihvaća [[Rasjed|koso klizanje]] i na kojoj se dogodio [[Velikog tsunami u Yaeyami 1771.]] godine.<ref>{{Cite journal|last=Bird|first=Peter|date=2003|title=An updated digital model of plate boundaries: UPDATED MODEL OF PLATE BOUNDARIES|journal=Geochemistry, Geophysics, Geosystems|language=en|volume=4|issue=3|doi=10.1029/2001GC000252|doi-access=free}}</ref><ref>{{Cite journal|last=Okamura|first=Yukinobu|last2=Nishizawa|first2=Azusa|last3=Fujii|first3=Yushiro|last4=Yanagisawa|first4=Hideaki|date=2018-09-11|title=Accretionary prism collapse: a new hypothesis on the source of the 1771 giant tsunami in the Ryukyu Arc, SW Japan|journal=Scientific Reports|volume=8|issue=1|pages=13620|doi=10.1038/s41598-018-31956-8|pmid=30206405|issn=2045-2322|pmc=6134009}}</ref> Sjeverna strana Okinawske ploče omeđena je [[Amurska ploča|Amurskom pločom]].
 == Izvori ==

Okinavska ploča: razlika između inačica

Posljednja izmjena od 1. svibanj 2022. u 04:24

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Izvori[uredi]

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