Scandinavian Caledonides

Location of the different branches of the Caledonian/Acadian belts at the end of the Caledonian orogeny (Early Devonian).[1][2][3][4][5] Present day coastlines are indicated in gray for reference. Note, that the North-German–Polish Caledonides were not formed during the Scandian orogeny but during the "soft docking" of East Avalonia to Baltica at about 443 Ma.[1][6][7] The Acadian orogeny resulted from the prolonged collision of the "peri-Gondwanan terranes" with the Laurentian autochthon.[1] Later in geological history, the North Atlantic Ocean opened[8][9][10] and the different parts of the orogenic belt moved apart. See also Iapetus Suture and Trans-European Suture Zone.

The Scandinavian Caledonides are the vestiges of an ancient, today deeply eroded orogenic belt formed during the SilurianDevonian continental collision of Baltica and Laurentia, which is referred to as the Scandian phase of the Caledonian orogeny.[11] The size of the Scandinavian Caledonides at the time of their formation can be compared with the size of the Himalayas.[12] The area east of the Scandinavian Caledonides, including parts of Finland, developed into a foreland basin where old rocks and surfaces were covered by sediments.[13] Today, the Scandinavian Caledonides underlie most of the western and northern Scandinavian Peninsula,[14][15] whereas other parts of the Caledonides can be traced into West and Central Europe as well as parts of Greenland[16] and eastern North America.

Plate-tectonic history

The Caledonian Wilson cycle commenced with the continental break-up of Rodinia[17] and the opening of the Iapetus ocean about 616–583 Ma (mega-annum) ago.[18][19][20] The Iapetus was at its widest in the Late CambrianEarly Ordovician[21][1] before it began to close by subduction of Iapetus crust along the Gondawanan and Laurentian margins starting between 500 and 488 Ma ago.[1][22][23] Subduction of Iapteus crust continued until about 430 Ma ago until the final continental collision of Laurentia with Baltica, i.e. the Scandian phase of the Caledonian orogeny. The time of the continental collision is estimated by the cessation of subduction-related magmatism and a common apparent polar wander path (APWP) for Laurentia and Baltica.[24][7]

During the collision, the Baltican continental margin was deeply subducted beneath Laurentia and eclogitized. The time of the maximal burial of the Baltican margin is estimated at 410 Ma ago by radiometric age dating of the ultra-high pressure (UHP) metamorphism in the Western Gneiss Region (WGR). Also during the collision, the Caledonian allochthons were thrust over the Baltican margin. Peak metamorphism in the allochthons is estimated to have occurred somewhat earlier than in the autochthon at about 420 Ma ago.

Following the subduction of the Baltican continental margin and thrusting of the nappes over the Baltican basement, the orogen began to collapse in the Early Devonian, which was associated with extensional tectonics[25][26] and sinistral motion between the Laurentian and Baltican tectonic plates.

Disposition of rocks

A conceptual NW-SE oriented cross section of the Scandinavian Caledonides near Torneträsk in northernmost Sweden. Each nappe is shown with a different colour. Arrows show the relative movement of each nappe. The décollement plane is shown as black dented line. Note the general movement towards the southeast.

The Caledonian orogeny put in place most of the bedrock now seen in the Scandinavian Mountains. Caledonian rocks overlie rocks of the much older Svecokarelian and Sveconorwegian provinces. The Caledonian rocks form large nappes (Swedish: skollor) that have been thrust over the older rocks. Much of the Caledonian rocks have been eroded since they were put in place meaning that they were once thicker and more contiguous. It is also implied from the erosion that the nappes of Caledonian rock originally reached further east than they do today. The erosion has left remaining massifs of Caledonian rocks and windows of Precambrian-aged rock.[27]

While there are some disagreements, geologists generally recognize four units among the nappes: an Uppermost, an Upper, a Middle and a Lower one.[28][A] The last one is made up Ediacaran (Vendian), Cambrian, Ordovician and Silurian-aged sedimentary rocks. Pieces of Precambrian shield rocks are in some places also incorporated into the Lower nappes.[27]

Present-day topography of Scandinavia

Despite occurring in roughly the same area, the ancient Scandinavian Caledonian Mountains and the modern Scandinavian Mountains are not synonymous. The overlap between the Scandinavian Caledonides and the Scandinavian Mountains has led to various suggestions that the modern Scandinavian Mountains are a remnant of the Caledonide mountains.[14][30] A version of this argument was put forward in 2009 with the claim that the uplift of the mountains was attained by buoyancy of the surviving "mountain roots" of the Caledonian orogen.[14] This concept has been criticized because there is only a tiny "mountain root" beneath the southern Scandinavian Mountains and no "root" at all in the north. Further, the Caledonian Mountains in Scandinavia are known to have undergone orogenic collapse for a long period starting in the Devonian.[14][31][26] Another problem with this model is that it does not explain why other former mountains dating back to the Caledonian orogeny are eroded and buried in sediments and not uplifted by their "roots".[14] Others claim that molten magma exists below the Caledonides of Norway, causing the uplift.[32]

See also

Notes

  1. ^ Corfu and coworkers assess the scheme as a "useful basis for further exploration" but regard it also as "too rigid and simplistic" since paleogeography is poorly represented.[29]

References

  1. ^ a b c d e Domeier, Mathew (2016). "A plate tectonic scenario for the Iapetus and Rheic oceans". Gondwana Research. 36: 275–295. Bibcode:2016GondR..36..275D. doi:10.1016/j.gr.2015.08.003. ISSN 1342-937X.
  2. ^ Torsvik, Trond; Smethurst, M.; Meert, J.; Van der Voo, Rob; McKerrow, W.; Brasier, M.; Sturt, Brian A.; Walderhaug, H. (1996). "Continental break-up and collision in the Neoproterozoic and Palaeozoic — A tale of Baltica and Laurentia". Earth-Science Reviews. 40 (3–4): 229–258. Bibcode:1996ESRv...40..229T. doi:10.1016/0012-8252(96)00008-6. ISSN 0012-8252.
  3. ^ Stampfli, G.M; Borel, G.D (2002). "A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons". Earth and Planetary Science Letters. 196 (1–2): 17–33. Bibcode:2002E&PSL.196...17S. doi:10.1016/s0012-821x(01)00588-x. ISSN 0012-821X.
  4. ^ Matte, P. (2001). "The Variscan collage and orogeny (480-290 Ma) and the tectonic definition of the Armorica microplate: a review". Terra Nova. 13 (2): 122–128. Bibcode:2001TeNov..13..122M. doi:10.1046/j.1365-3121.2001.00327.x. ISSN 0954-4879. S2CID 129727506.
  5. ^ Ziegler, P. A. (1990). Geological Atlas of Western and Central Europe. Shell Internationale Petroleum Maatschappij BV/Geological Society of London.
  6. ^ Torsvik, Trond H.; Rehnström, Emma F. (2003). "The Tornquist Sea and Baltica–Avalonia docking". Tectonophysics. 362 (1–4): 67–82. Bibcode:2003Tectp.362...67T. doi:10.1016/s0040-1951(02)00631-5. ISSN 0040-1951.
  7. ^ a b Torsvik, Trond H.; Van der Voo, Rob; Preeden, Ulla; Mac Niocaill, Conall; Steinberger, Bernhard; Doubrovine, Pavel V.; van Hinsbergen, Douwe J.J.; Domeier, Mathew; Gaina, Carmen (2012). "Phanerozoic polar wander, palaeogeography and dynamics". Earth-Science Reviews. 114 (3–4): 325–368. Bibcode:2012ESRv..114..325T. doi:10.1016/j.earscirev.2012.06.007. hdl:10852/62957. ISSN 0012-8252.
  8. ^ Mosar, Jon; Eide, Elizabeth A.; Osmundsen, Per Terje; Sommaruga, Anna; Torsvik, Trond H. (2002). "Greenland-Norway separation: A geodynamic model for the North Atlantic". Norwegian Journal of Geology. 82: 281–298.
  9. ^ Gaina, Carmen; Gernigon, L.; Ball, P. (2009). "Palaeocene–Recent plate boundaries in the NE Atlantic and the formation of the Jan Mayen microcontinent". Journal of the Geological Society. 166 (4): 601–616. Bibcode:2009JGSoc.166..601G. doi:10.1144/0016-76492008-112. ISSN 0016-7649. S2CID 128700588.
  10. ^ Seton, Maria; Müller, R.D.; Zahirovic, S.; Gaina, Carmen; Torsvik, Trond H.; Shephard, Grace; Talsma, A.; Gurnis, M.; Turner, M. (2012). "Global continental and ocean basin reconstructions since 200 Ma". Earth-Science Reviews. 113 (3–4): 212–270. Bibcode:2012ESRv..113..212S. doi:10.1016/j.earscirev.2012.03.002. ISSN 0012-8252.
  11. ^ Corfu, F.; Andersen, T. B.; Gasser, D. (2014). "The Scandinavian Caledonides: main features, conceptual advances and critical questions". Geological Society, London, Special Publications. 390 (1): 9–43. Bibcode:2014GSLSP.390....9C. doi:10.1144/sp390.25. ISSN 0305-8719. S2CID 128630362.
  12. ^ Labrousse, Loïc; Hetényi, György; Raimbourg, Hugues; Jolivet, Laurent; Andersen, Torgeir B. (2010). "Initiation of crustal-scale thrusts triggered by metamorphic reactions at depth: Insights from a comparison between the Himalayas and Scandinavian Caledonides" (PDF). Tectonics. 29 (5): n/a. Bibcode:2010Tecto..29.5002L. doi:10.1029/2009tc002602. ISSN 0278-7407.
  13. ^ Murrell, G.R.; Andriessen, P.A.M. (2004). "Unravelling a long-term multi-event thermal record in the cratonic interior of southern Finland through apatite fission track thermochronology". Physics and Chemistry of the Earth, Parts A/B/C. 29 (10): 695–706. Bibcode:2004PCE....29..695M. doi:10.1016/j.pce.2004.03.007.
  14. ^ a b c d e Green, Paul F.; Lidmar-Bergström, Karna; Japsen, Peter; Bonow, Johan M.; Chalmers, James A. (2013). "Stratigraphic landscape analysis, thermochronology and the episodic development of elevated, passive continental margins". Geological Survey of Denmark and Greenland Bulletin. 30: 18. doi:10.34194/geusb.v30.4673. Retrieved 30 April 2015.
  15. ^ Gabrielsen, Roy H.; Faleide, Jan Inge; Pascal, Christophe; Braathen, Alvar; Nystuen, Johan Petter; Etzelmuller, Bernd; O'Donnel, Sejal (2010). "Latest Caledonian to Present tectonomorphological development of southern Norway". Marine and Petroleum Geology. 27 (3): 709–723. Bibcode:2010MarPG..27..709G. doi:10.1016/j.marpetgeo.2009.06.004.
  16. ^ Haller, J. (1985). "The East Greenland Caledonides—reviewed". The Caledonide Orogen—Scandinavia and Related Areas: 1031–1046.
  17. ^ Torsvik, Trond H.; Cocks, L. Robin M. (2016), "Earth's Origins and the Precambrian", Earth History and Palaeogeography, Cambridge University Press, pp. 77–84, doi:10.1017/9781316225523.005, ISBN 9781316225523
  18. ^ Meert, Joseph G.; Torsvik, Trond H.; Eide, Elizabeth A.; Dahlgren, Sven (1998). "Tectonic Significance of the Fen Province, S. Norway: Constraints From Geochronology and Paleomagnetism". The Journal of Geology. 106 (5): 553–564. Bibcode:1998JG....106..553M. doi:10.1086/516041. ISSN 0022-1376. S2CID 129740587.
  19. ^ Bingen, B.; Demaiffe, D.; Breemen, O. van (1998). "The 616 Ma Old Egersund Basaltic Dike Swarm, Sw Norway, and Late Neoproterozoic Opening of the Iapetus Ocean". The Journal of Geology. 106 (5): 565–574. Bibcode:1998JG....106..565B. doi:10.1086/516042. ISSN 0022-1376. S2CID 59043758.
  20. ^ Svenningsen, O (2001). "Onset of seafloor spreading in the Iapetus Ocean at 608 Ma: precise age of the Sarek Dyke Swarm, northern Swedish Caledonides". Precambrian Research. 110 (1–4): 241–254. Bibcode:2001PreR..110..241S. doi:10.1016/s0301-9268(01)00189-9. ISSN 0301-9268.
  21. ^ Torsvik, Trond H.; Cocks, L. Robin M. (2016), "Ordovician", Earth History and Palaeogeography, Cambridge University Press, pp. 101–123, doi:10.1017/9781316225523.007, ISBN 9781316225523
  22. ^ Dunning, G. R.; Pedersen, R. B. (1988). "U/Pb ages of ophiolites and arc-related plutons of the Norwegian Caledonides: implications for the development of Iapetus". Contributions to Mineralogy and Petrology. 98 (1): 13–23. Bibcode:1988CoMP...98...13D. doi:10.1007/bf00371904. ISSN 0010-7999. S2CID 129115454.
  23. ^ Slagstad, Trond; Pin, Christian; Roberts, David; Kirkland, Christopher L.; Grenne, Tor; Dunning, Greg; Sauer, Simone; Andersen, Tom (2013). "Tectonomagmatic evolution of the Early Ordovician suprasubduction-zone ophiolites of the Trondheim Region, Mid-Norwegian Caledonides". Geological Society, London, Special Publications. 390 (1): 541–561. doi:10.1144/sp390.11. ISSN 0305-8719. S2CID 129082705.
  24. ^ Corfu, F.; Torsvik, T.H.; Andersen, T.B.; Ashwal, L.D.; Ramsay, D.M.; Roberts, R.J. (2006). "Early Silurian mafic-ultramafic and granitic plutonism in contemporaneous flysch, Mageroy, northern Norway: U-Pb ages and regional significance". Journal of the Geological Society. 163 (2): 291–301. Bibcode:2006JGSoc.163..291C. CiteSeerX 10.1.1.521.6893. doi:10.1144/0016-764905-014. ISSN 0016-7649. S2CID 19071114.
  25. ^ Andersen, Torgeir B. (1998). "Extensional tectonics in the Caledonides of southern Norway, an overview". Tectonophysics. 285 (3–4): 333–351. Bibcode:1998Tectp.285..333A. CiteSeerX 10.1.1.571.80. doi:10.1016/s0040-1951(97)00277-1. ISSN 0040-1951.
  26. ^ a b Dewey, J.F.; Ryan, P.D.; Andersen, T.B. (1993). "Orogenic uplift and collapse, crustal thickness, fabrics and metamorphic phase changes: the role of eclogites". Geological Society, London, Special Publications. 76 (1): 325–343. Bibcode:1993GSLSP..76..325D. doi:10.1144/gsl.sp.1993.076.01.16. S2CID 55985869.
  27. ^ a b Lundqvist, Jan; Lundqvist, Thomas; Lindström, Maurits; Calner, Mikael; Sivhed, Ulf (2011). "Fjällen". Sveriges Geologi: Från urtid till nutid (in Swedish) (3rd ed.). Spain: Studentlitteratur. pp. 323–340. ISBN 978-91-44-05847-4.
  28. ^ Stephens, M. B.; Gee, David G. (1985). "A tectonic model for the evolution of the eugeoclinal terranes in the central Scandinavian Caledonides". The Caledonide Orogen—Scandinavia and Related Areas: 954–978.
  29. ^ Corfu, F.; Andersen, T.B.; Gasser, D. (2014). "The Scandinavian Caledonides: main features, conceptual advances and critical questions". New Perspectives on the Caledonides of Scandinavia and Related Areas. Geological Society, London, Special Publications. Vol. 390. pp. 9–43. Bibcode:2014GSLSP.390....9C. doi:10.1144/SP390.25. S2CID 128630362.
  30. ^ Schiffer, Christian; Balling, Neils; Ebbing, Jörg; Holm Jacobsen, Bo; Nielsen, Søren Bom (2016). "Geophysical-petrological modelling of the East Greenland Caledonides – Isostatic support from crust and upper mantle". Tectonophysics. 692: 44–57. doi:10.1016/j.tecto.2016.06.023.
  31. ^ Chalmers, J.A.; Green, P.; Japsen, P.; Rasmussen, E.S. (2010). "The Scandinavian mountains have not persisted since the Caledonian orogeny. A comment on Nielsen et al. (2009a)". Journal of Geodynamics. 50 (2): 94–101. Bibcode:2010JGeo...50...94C. doi:10.1016/j.jog.2010.02.001.
  32. ^ "The lost volcanoes of Norway". 11 April 2018.

Read other articles:

Typhoon Babs (Loleng) to the east of the Philippines in October 1998 The Philippines is archipelagic country in Southeast Asia, located in the northwest Pacific Ocean. It consists of 7,641 islands. The country is known to be the most exposed country in the world to tropical storms, with about twenty tropical cyclones entering the Philippine area of responsibility each year. In the Philippine languages, tropical cyclones are generally called bagyo.[1] Climatologically, in the Northwest...

 

 

This article relies largely or entirely on a single source. Relevant discussion may be found on the talk page. Please help improve this article by introducing citations to additional sources.Find sources: Dear John Hank Williams song – news · newspapers · books · scholar · JSTOR (May 2021) 1951 single by Hank Williams With His Drifting CowboysDear JohnSingle by Hank Williams With His Drifting CowboysB-sideCold, Cold HeartReleasedFebruary 2, 1951&#...

 

 

This article needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed.Find sources: Meløyvær Fortress – news · newspapers · books · scholar · JSTOR (November 2022) (Learn how and when to remove this template message) Meløyvær fortKrøttøya, Norway Meløyvær Fortress Canon B - Russøya (Meløyvær)Meløyvær fortCoordinates69°03′30″N...

المشتري المشتري نظام المشتري [الإيطالية] المحددات المداريّة [الإيطالية] التكوّن [الإيطالية] الغلاف الجوي البقعة الحمراء العظيمة البنية الداخليّة [الإيطالية] الغلاف المغناطيسي الحلقات الأقمار طروادة مشترية حوادث التصادم [الإيطالية] الرصد [الإيطالية] الاستكشاف في الأدب ال...

 

 

This article may need to be rewritten to comply with Wikipedia's quality standards. You can help. The talk page may contain suggestions. (July 2015) 2011 video gameTales of the World: Radiant Mythology 3Developer(s)Alfa SystemPublisher(s)NamcoComposer(s)Takuya YasudaKota NakashimaMotoi SakurabaKazuhiro NakamuraGo ShiinaSeriesTalesPlatform(s)PlayStation PortableReleaseJP: February 10, 2011Genre(s)Action RPGMode(s)Single-player Tales of the World: Radiant Mythology 3 (テイルズオブザワー

 

 

За вітриною універмагурос. За витриной универмага Жанр комедіяРежисер Самсон СамсоновСценарист Олексій Каплер Самсон СамсоновУ головних ролях Іван Дмитрієв Наталія МедведєваОператор Федір Добронравов Володимир МонаховКомпозитор Олександр ЦфасманХудожник Борис Че...

Perang Romawi Timur-Bulgariake kanan searah jarum jam: Pertempuran Ankhialos; Khan Omurtag; Para Kaisar Bulgaria dan Romawi Timur menegosiasikan perdamaian; Kaisar Nikephoros II Phokas.Tanggal680–1355 MLokasiSemenanjung BalkanHasil Utsmaniyah mengasai BalkanPerubahanwilayah Kedua kekaisaran mengalami perubahan wilayahPihak terlibat Kekaisaran Bulgaria PertamaKekaisaran Bulgaria Kedua Kekaisaran Romawi TimurTokoh dan pemimpin AsparukhTervelKormisoshVinekhTeletsTelerigKrumOmurtagMalamirPresia...

 

 

2018 film directed by Abhishek Kapoor KedarnathTheatrical release posterDirected byAbhishek KapoorWritten byKanika DhillonAbhishek KapoorBased onThe Kedarnath FloodsProduced byRonnie ScrewvalaPragya KapoorAbhishek KapoorStarringSushant Singh RajputSara Ali KhanCinematographyTushar Kanti RayEdited byChandan AroraMusic byScore:Hitesh SonikSongs:Amit TrivediProductioncompaniesRSVP MoviesGuy in the Sky PicturesDistributed byRSVP MoviesRelease date 7 December 2018 (2018-12-07) Runni...

 

 

У этого термина существуют и другие значения, см. Тюрьма (значения). Зиндан. Бухара, 1915 Коридор в Багдадской центральной тюрьме (Абу-Грейб, Ирак) Заключённые в Папуа — Новой Гвинее (март, 2013 год) Тюрьма́ (по разным версиям, от немецкого Turm — башня, тюркского türme или от та...

Public university in Atlanta, Georgia, US Georgia Institute of TechnologyFormer nameGeorgia School of Technology (1885–1948)MottoProgress and ServiceTypePublic research universityEstablishedOctober 13, 1885; 138 years ago (1885-10-13)[1]Parent institutionUniversity System of GeorgiaAccreditationSACSAcademic affiliationAAUGRAORAUURASpace-grantEndowment$2.97 billion (2021)[2]Budget$2.12 billion (2021)[3]PresidentÁngel CabreraProvostSteven McLaughlin&...

 

 

Este artículo o sección necesita referencias que aparezcan en una publicación acreditada.Este aviso fue puesto el 7 de enero de 2017. Fuego y poesíaÁlbum de estudio de Xulio FormosoPublicación 1977Grabación FidelisFormato Vinilo 33rpm LPDiscográfica PolydorProductor(es) Xulio Formoso Cronología de Xulio Formoso Levántate Rosalía ((1976)) Fuego y poesía ((1977)) Soles y centauros ((1977)) [editar datos en Wikidata]Fuego y poesía surgió en respuesta a una propuesta concr...

 

 

For other uses, see Otelo. This article needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed.Find sources: Otelo Burning – news · newspapers · books · scholar · JSTOR (May 2014) (Learn how and when to remove this template message) 2011 South African filmOtelo BurningTheatrical release posterDirected bySara BlecherScreenplay byJames WhyleSa...

Railway station in Kawachinagano, Osaka Prefecture, Japan Amami Station天見駅Amami Station, July 2007General informationLocation195-1, Amami, Kawachinagano-shi, Osaka-fu 586-0062JapanCoordinates34°23′48.5″N 135°35′43.3″E / 34.396806°N 135.595361°E / 34.396806; 135.595361Operated by Nankai Electric RailwayLine(s) Koya LineDistance34.9 km from ShiomibashiPlatforms2 side platformsConnections Bus terminal Other informationStation codeNK73WebsiteOfficial webs...

 

 

2014 protest movement in Taiwan Sunflower Student MovementDateMarch 18 – April 10, 2014 (2014-03-18 – 2014-04-10) (23 days)LocationLegislative YuanZhongzheng District, Taipei City, Taiwan25°2′39.8832″N 121°31′10.02″E / 25.044412000°N 121.5194500°E / 25.044412000; 121.5194500Caused byCross-Strait Service Trade AgreementGoals Halt the enforcement of Cross-Strait Service Trade Agreement Legislate supervision on cross-strait ag...

 

 

Indian actor This biography of a living person needs additional citations for verification. Please help by adding reliable sources. Contentious material about living persons that is unsourced or poorly sourced must be removed immediately from the article and its talk page, especially if potentially libelous.Find sources: Rajat Bedi – news · newspapers · books · scholar · JSTOR (August 2012) (Learn how and when to remove this template message) Rajat Bed...

Third annual Australian Rules football national competition 1914 Sydney CarnivalTournament informationSportAustralian footballLocationSydney, AustraliaDates5 August 1914–15 August 1914FormatRound RobinTeams6Final championVictoria← 19111921 → New South Wales vs South Australia at the SCG Victoria vs Western Australia at the SCG The 1914 Sydney Carnival was the third edition of the Australian National Football Carnival, an Australian football interstate competition. It w...

 

 

The examples and perspective in this article deal primarily with the United Kingdom and do not represent a worldwide view of the subject. You may improve this article, discuss the issue on the talk page, or create a new article, as appropriate. (December 2023) (Learn how and when to remove this template message) Guideline governing legal pleas of insanity Daniel M'Naghten c. 1856 The M'Naghten rule(s) (pronounced, and sometimes spelled, McNaughton) is a legal test defining the defence o...

 

 

Mozilla Jetpack開發者Mozilla公司Mozilla基金會编程语言HTML、CSS、JavaScript引擎Gecko操作系统跨平台类型軟體開發套件(SDK)许可协议MPL网站wiki.mozilla.org/Jetpack Mozilla Jetpack是一個實驗性的Firefox附加元件平台,可以使用HTML、CSS和JavaScript簡單語法來開發新功能,並且安裝附加元件后不用重新啟動瀏覽器即可使用,也消除了Firefox舊有架構常与附加元件版本出现的相容性問題[1]。 這...

Ella-Rae Smith Ella-Rae Smith en una entrevista en 2022Información personalNombre completo Ella Rae Kirby-SmithNacimiento 21 de febrero de 1998 (26 años) Bristol (Reino Unido)Nacionalidad BritánicaLengua materna InglésCaracterísticas físicasAltura 1,77 m (5′ 10″)Peso 55 kg (121 lb)Ojos AzulesCabello CastañoEducaciónEducada en Cotham SchoolInformación profesionalOcupación Actriz modeloAños activa 2016–presente[editar datos en Wikidata] Ella-Rae Kirby-S...

 

 

جزء من سلسلة مقالات حولالمحاسبة الأنواع الرئيسية تدقيق موازنة تكاليف جنائية مالية التمويل عامة إدارية اجتماعية ضريبية المفاهيم الأساسية الفترة المحاسبية تزايد القوة الشرائية الثابتة كيان اقتصادي قيمة عادلة فرض الاستمرارية التكلفة التاريخية مبدأ المقابلة الأهمية النس...

 

 

Strategi Solo vs Squad di Free Fire: Cara Menang Mudah!