| A | B | C | D | E | F | G | H | I | J | K | L | M | N | O | P | Q | R | S | T | U | V | W | X | Y | Z | |
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1 | Evidence for Formation in Island Arc Setting | |||||||||||||||||||||||||
2 | Locality | Location | Orogen/Province | Age (Ma) | ± | Methods/Refs. | Lithologies included in compilation | Metamorphism (facies) | Tectonic setting interpretation of previous studies | Field Relationships/ Regional Geology | Geochronology (supporting tectonic history as island arc) | Trace Elements (arc-like signature) | Boninites Present | Fe3+/FeT | V/Sc | |||||||||||
3 | Western Aleutian Arc | Piip volcano & dredges near Komandorsky Islands | - | 11.5 | 11.5 | Miocene to Holocene (0-23 Ma). (Yogodzinski et al., 1995 GSAB, 107: 505-519) | basalts and andesites | - | active island arc | Y | ||||||||||||||||
4 | Kuril Arc | - | 12.5 | 12.5 | less than 25 million years based on tectonic history | basalts and andesites | - | active island arc | Y | |||||||||||||||||
5 | Tonga Arc | - | 23 | 23 | given age range in Hergt and Woodhead, 2007 Chem. Geol., 245: 9-44. | basalts to dacites | - | active island arc | Y | |||||||||||||||||
6 | Uasilau-Yau Yau intrsuive complex | New Britain, Papua New Guinea | - | 28.4 | 0.6 | K-Ar age on seven hornblendes (Whalen, 1985, J Petrology, 26:603-632) | gabbro to granodiorite | - | plutonic rocks related to recent intra-oceanic arc magmatism | X | X | X | Y | Y | ||||||||||||
7 | South Shetland Islands, Antarctica | King George Island and Livingston Island | - | 72 | 58 | average of maximum and minimum ages given in Birkenmajer et al., 1991 Antarctic Sci., 3: 293-308 | volcanic, hypabyssal, and intrusive rocks of basaltic to andesitic composition | - | intra-oceanic arc | X | X | X | Y | Y | ||||||||||||
8 | Kohistan-Ladakh paleo-arc | NW Pakistan | Neo-tethyan orogen | 85 | 35 | subduction initiation around 120 Ma and final collision with India at 50 Ma (see Bouilhol et al., 2013, EPSL 366:163-175) | volcanic rocks of basaltic to dacitic in composition; amphibolites; gabbros; diorites | variable | intra-oceanic arc | X | X | X | X | Y | Y | |||||||||||
9 | Kizildag ophiolite | Turkey | peri-Arabian ophiolite belt | 91.7 | 0.1 | multi-zircon U-Pb TIMS age from plagiogranite (Dilkek and Thy, 2009, Lithos: 113, 68-87) | gabbros, sheeted dikes, basalts to basaltic andesite pillow lavas | - | suprasubduction zone ophiolite | X | X | X | X | Y | ||||||||||||
10 | Téneme formation, Mayarí-Cristal ophiolitic massif | Cuba | - | 91.9 | 2.1 | associated fossil assemblage dated to Turonian to early Coniacian. Cross-cut by quartz-diorite dated at 89.7 Ma. (Proenza et al. 2006, Geologica Acta, 4(1-2):103-121.) | intrusive and extrusive rocks of tholeiitic basalt to basaltic andesite in composition | - | primitive intra-oceanic arc | X | Y | |||||||||||||||
11 | Pekulney-Zolotogorskaya paleo-arc | Chukotka Peninsula, NE Russia | - | 138 | 8 | Neocomian (based on field relationships with olistostrome blocks) | gabbro, tholeiitic basalts, tonalites, plagiogranites | greenschist | intra-oceanic arc | X | X | Y | ||||||||||||||
12 | Coast Range volcanic rocks | Central Chile | - | 150.7 | 50.7 | Early Jurassic to Early Cretaceous | basalts to basaltic andesites | prehnite-pumpellyite | intra-oceanic arc | X | X | Y | ||||||||||||||
13 | San Andres-Cedros complex | Baja, Mexico | - | 153.5 | 37.2 | average of U-Pb zircon ages of San Andres magmatic arc granitoids (Kimborough & Moore, 2003 GSA Spec. Pap, 374) | plutonics rocks (gabbros to granites) | - | intra-oceanic arc off-board continent | X | X | X | Y | Y | ||||||||||||
14 | Talkeetna paleo-arc | Alaska, USA | Western Cordillera | 185 | 15 | Volcanic rock ranges of ~200 to 170 Ma based on fossil records (see Clift et al., 2005 GSAB, 117: 902-925). Plutonic rocks yield similar range in U-Pb zircon ages. (Rioux et al., 2007, GSA Bulletin, 119:1168-1184) | intermediate to felsic plutonic rocks, basaltic to rhyolitic volcanic rocks | variable | intra-oceanic arc | X | X | X | Y | Y | ||||||||||||
15 | Bangong–Nujiang suture zone | Central Tibet | Tibetan Plateau | 220 | 2.1 | Average of LA-ICP-MS U-Pb zircon ages for Amdo pillow lavas (Chen et al., 2005 Lithos, 230: 30-45.) | Pillow lavas (Amdo area) | - | intra-oceanic arc to back arc basin | X | X | X | X | Y | Y | |||||||||||
16 | Brook Street terrane (Plato and Largs terranes) | South Island, New Zealand | 275.4 | 23.5 | Permian, based on intercalations of Atomodesmatinid limestones | Basaltic dikes (Plato Terrane). Andesitic to dacitic volcanics (Largs terrane) | prehnite-pumpellyite to lower greenschist | paired system of intra-oceanic arcs | X | X | Y | |||||||||||||||
17 | Ailaoshan-Song Ma tectonic zone (Wusu and Yaxuanqiao basalts) | Western Yunan, China | 276 | 11 | SHRIMP U-Pb zircon age (average of the Wusu and Yaxuanqiao basalts) (Fan et al. 2010, Lithos, 119:553-568) | basalts of the Wusu and Yaxuanqiao formations | - | intra-oceanic arc to back arc basin | X | X | X | Y | ||||||||||||||
18 | Hugiert-Chaganhadamiao volcanic-plutonic sequence | China | Solonker suture zone, Central Asian Orogenic Belt | 284 | 4 | U-Pb zircon from associated gabbro and plagiogranite (Jian et al., 2010, Lithos, 118:169-190). | basalts | greenschist | intra-oceanic arc | X | X | X | Y | |||||||||||||
19 | Changning-Menglian, Gicha, and Banpo sequences | Southwestern China | Paleo-Tethys orogen | 287.5 | 23.5 | Range of ages given for sequences in Jian et al. 2009, Lithos, 113: 748-766. | mostly basalts and gabbros (minor tonalite and hornblendite) | - | several intra-oceanic arcs to back arc basins | X | X | X | Y | |||||||||||||
20 | Zharma-Saur terrane | eastern Kazakhstan | Central Asian Orogenic Belt | 313 | 2.1 | Best estimate of Li et al, 2015, J. of Asian Earth Sciences, 113:16-35. based on SIMS U-Pb zircon age analysis. | basalts | - | intra-oceanic arc | X | X | X | Y | |||||||||||||
21 | New England Orogen | Australia | 377.5 | 5.3 | Late Devonian (see Offler and Murray, 2011, Gond. Res. 19:706-715. | volcanic rocks of basaltic to dacitic in composition. | prehnite-pumpellyite | intra-oceanic arc | X | X | Y | Y | ||||||||||||||
22 | Junggar terrane | Xinjiang Province, China | Central Asian Orogenic Belt | 396.5 | 11.5 | Tuoranggekuduke Fm. age of 408 Ma (method not specified). Beitashan Fm. Is middle Devonian based on fossils. (Zhang et al. 2008, Lithos, 105:379-395.) | basalts to andesites | greenschist | intra-oceanic arc | X | X | Y | Y | |||||||||||||
23 | Copley Greenstone | Klamath Mountains, Oregon, USA | Sierran-Klamath Orogen | 406 | 13 | Early Devonian based on age of overlying strata (Lapierre et al. 1985, Can. J. of Earth Sci. 22(2): 214-226) | basalt to andesite | greenschist | immature intra-oceanic arc | X | X | X | Y | |||||||||||||
24 | North Qinling–Tongbai orogen | China | Qingling-Tongbai-Dabie-Sulu orogenic belt | 441.5 | 1.5 | LA-ICP-MS U-Pb zircon age (Wang et al., 2013 Lithos, 179: 1-15) | Erlangping gabbros | - | back-arc basin | X | X | Y | ||||||||||||||
25 | Kingston terrane | New Brunswick, Canada | Taconic orogeny | 442 | 6 | TIMS U-Pb zircon age or related dacitic tuff unit, (Barr et al., 2002, Geol. Soc. Am. Bull. 114:964-982) | Kingston group dikes (mafic and silicic) | upper greenschist to lower amphibolite | extension related magmatism in an intra-oceanic arc | X | X | X | Y | Y | ||||||||||||
26 | Fan–Karategin metamorphic belt | Tajikstan | Central Asian Orogenic Belt | 443.8 | 12.5 | Given as "upper ordovician-lower silurian", taken as Ordovician/Silurian boundary, arbitrary ±12.5 myr used (Volkova and Budanov, 1999, Lithos, 47:201-216) | andesites, dacite, and rhyolite (of Norvat series) | greenschist | intra-oceanic arc | X | X | Y | ||||||||||||||
27 | Macquarie Arc | New South Wales, Australia | Lachlan orogen | 452.5 | 12.5 | Average of max/min ages given in Crawford et al., 2007 Aust. J. of Ear. Sci., 54: 181-214. | volcanic and plutonic rocks of broad compositional range. Mostly basalts and andesites. | - | intra-oceanic arc | X | X | X | Y | |||||||||||||
28 | Bronson Hill arc | Connecticut, Massachusetts, and New Hampshire, USA | Taconic orogeny | 448 | 8 | best estimate of magmatism based on range of ages reported in literature from Karabinos et al., 2017, Amer. J. of Sci., 317:515-554. | Ammonoosuc volcanics: metamorphosed tholeiitic basalt, andesite, low-K dacite, and rhyolite | amphibolite facies | arc marginal to Laurentia | X | X | X | Y | |||||||||||||
29 | Shangdan and Erlangping belts | China | Qingling orogenic belt | 467 | 47 | See broad range of arc-related magmatism ages based on U-Pb dating in zircons from various units in the Qingling area (Dong et al. 2011. Lithos, 122: 39-56) | basalts to andesites, gabbros | - | intra-oceanic arc to back arc basin | X | X | X | Y | |||||||||||||
30 | Lough Nafooey arc | Ireland | Grampian (Irish Caledonides) | 482 | 7 | Average of max/min ages given in Ryan and Dewey, 2011. In Arc-Continent Collision (pp. 373-401). Springer, Berlin, Heidelberg. | Bohaun Group (boninite pillows, earliest young subduction zone) and lower Lough Nafooey Group (tholeiitic pillow basalts and breccia) | - | arc-related volcanism that spans the Grampian arc-continent collision event. | X | X | X | X | Y | ||||||||||||
31 | Penobscot and Victoria arcs | Newfoundland, Canada | Taconic orogeny, Appalachians | 483 | 30 | average of max/min age ranges give for Penobscot Arc (c. 513-486) and Victoria Arc 9c. 473-454) (Zagorevski, 2007 AJS, 307: 339-370) | Wild Bight group volcanics (Dominantly tholeiitic basalts, low-K rhyolites occur locally) and pillow basalts, basalts, and gabbro from Pats Pond and Wigwam Brook groups | - | intraoceanic arcs (though see also model of Zagorevski et al., 2007 suggesting ensialic orogen) | X | X | X | Y | Y | ||||||||||||
32 | Devil River arc, Takaka Terrane | South Island, New Zealand | 485 | 8 | SHRIMP U-Pb zircon age (Heath Volcanic suite, Benson volcanics. 515±7 Ma, SHRIMP U-Pb zircon age also given for Cobb Igneous Complex boninites. (Münker & Cooper, 1999, New Zealand J. of Geol. And Geophys. 103: 687-700). | Basalts to basaltic andesites with less common dacites to rhyolites. Boninites in the Cobb igneous complex formation. | prehnite-pumpellyite | intra-oceanic arc | X | X | X | X | Y | Y | ||||||||||||
33 | Heishan mafic-ultramafic complex | Qimantag Mountains, China | Eastern Kunlun Orogen | 486 | 6 | SHRIMP U-Pb zircon age (Meng et al, 2015, Gond. Res. 27: 745-759.) | gabbro and tholeiitic pillow basalts | - | intra-oceanic arc | X | X | X | Y | Y | ||||||||||||
34 | Bozshakol volcanic rocks | Kazakhstan | Central Asian Orogenic Belt | 501.8 | 3.2 | SIMS U-Pb zircon age | Tholeiitic to calc-alkaline basalt. Calc-alkaline andesite and dacite. Boninites. | - | intra-oceanic arc | X | X | X | X | Y | ||||||||||||
35 | Dariv arc | Mongolia | Central Asian Orogenic Belt | 503 | 0.3 | CA-ID-TIMS U-Pb zircon age (Bucholz et al., Geology, 2017, 45: 11-14) | Monzogabbros to quartz monzonites. Mafic to felsic dikes. | - | arc-related magmatism | X | X | X | Y | |||||||||||||
36 | Lushs Bight oceanic tract | Newfoundland, Canada | Taconic orogeny | 505.5 | 4.5 | Middle to Upper Cambrian (see van Staal et al. 2007, Geol. Soc. Amer. Mem. 200). | basalts and andesites of Long Island in Notre Dame Bay | - | immature intra-oceanic arc | X | X | X | X | Y | ||||||||||||
37 | Heathcote greenstone belt | Victoria, Australia | Lachlan orogen | 513.2 | 27.8 | Cambrian (Nelson et al., 1984 Cont. Min. Petrol., 88: 164-172) | tholeitic basalts and boninites | prehnite-pumpellyite to lower greenschist facies | intra-oceanic arc | X | Y | |||||||||||||||
38 | Uda-Vitim paleo-arc | Russia | 525 | 9 | 516-534 Ma range in U-Pb zircon ages (Gordienko et al., 2010 Russ. Geol. and Geophys. 51: 461-481) | basaltic, andesitic, basaltic andesitic, and dacitic lavas. | X | X | X | Y | ||||||||||||||||
39 | Dzhida paleo-arc | Mongolia | Central Asian Orogenic Belt | 540 | 30 | Range of U-Pb zircon ages from multiple samples; (Gordienko et al., 2006 Rus. Geol. Geophys, 47: 948-955) | Tholeiitic and bonninitic basalt flows and pillows. | greenschist | intra-oceanic arc | X | X | X | X | Y | Y | |||||||||||
40 | Khantaishir | Mongolia | Central Asian Orogenic Belt | 568 | 4 | U-Pb zircon age (Gibsher et al., 2001 Rus. Geol Geophys., 42: 1110-1117) | Sheeted dikes overlain by tholeiitic basalt and basaltic-andesite pillow lavas. | greenschist | Supra-subduction zone ophiolite formed in fore-arc rift environment. | X | X | X | X | Y | ||||||||||||
41 | Agardagh Tes-Chem ophiolite | Mongolia | Central Asian Orogenic Belt | 570 | 2 | U-Pb zircon age (Pfänder et al, 1998, Geol Surv Finland Spec Pap 26:42) | basalt, basaltic-andesite, andesite. Minor gabbro. | - | intra-oceanic arc | X | X | X | Y | |||||||||||||
42 | Dzela complex | Polar Urals, Russia | 578 | 8 | SIMS U-Pb zircon age (Remizov and Pease, 2004. Geol. Soc. Lond. Mem., 30:107-123) | basalt | greenschist overprinting blueschist, as well as, amphibolite | intra-oceanic arc | X | X | X | Y | ||||||||||||||
43 | Uimen-Lebed paleo-arc, Kurai-Ulagan, Gorny-Altai terrane | Russia | Central Asian Orogenic Belt | 622.5 | 24.5 | age range given in Safonova et al., 2017 Gondwana Res., 50: 167-194 | basalt, porphyritic basalt, gabbro | amphibolite | intra-oceanic arc | X | X | X | Y | |||||||||||||
44 | Bou Azzer-El Graara ophiolite | Anti-Atlas mountains, Morocco | 658 | 8 | SHRIMP U-Pb zircon age (Blein et al., 2014 J. Afr. Ear. Sci., 99: 287-306) | basalts, basaltic to andesitic dikes | greenschist to lower epitode-amphibolite | forearc | X | X | X | Y | ||||||||||||||
45 | Tilemsi paleo-arc | Mali | 726 | 7 | U-Pb zircon age (Caby et al., 1989 Can. J. Ear. Sci., 26: 1136-1146) | plutonic and volcanic rocks of basaltic to andesitic bulk composition | greenschist | intra-oceanic arc | X | X | X | Y | ||||||||||||||
46 | Central and South Eastern Desert of Egypt | Egypt | Arabian-Nubian shield; Pan-African orogen | 734 | 7 | SHRIMP U-Pb zircon age from Wadi el Dabbah metandesite (youngest concordant grain; Ali et al. PR, 2009) | basalts, andesites, and dacites of Wadi Hodein, Wadi Ranga, and Wadi el Dabbah | greenschist | intra-oceanic arc | X | X | X | Y | Y | ||||||||||||
47 | Adwa and Adi Nebrid Block | Axum Area, Ethiopia | Nafka terrane, Arabian Nubian Shield | 800 | 100 | broad range given by Tadesse et al., 1999 Precam. Res. 99: 101-124 | basalts, andesites, dacites, and rhyolites | greenschist | intra-oceanic arc | X | X | X | Y | |||||||||||||
48 | Yanbian Terrane | Sichuan Province, China | Yangtze block | 809 | 3 | Average SHRIMP U-Pb zircon age from Gaojiacun and Lengshuiqing intrusions (Zhou et al., 2006 Precam. Res., 144: 19-38) | Gaojiacun intrusion: gabbros to diorites. Lengshuiqing body: diorite, gabbro, and granodiorite to granite | - | intra-oceanic arc | X | X | X | Y | |||||||||||||
49 | Sibao arc | Guangxi, China | Jiangnan orogenic belt | 828 | 7 | SHRIMP U-Pb zircon age (see Zhou et al., 2004, Geochemical Journal, 38: 139-152) | basalt, andesite, diorite, gabbro | greenschist | intra-oceanic arc | X | X | Y | ||||||||||||||
50 | Wuyi-Yunkai domain | China | South China block | 976.5 | 7.5 | range in SHRIMP U-Pb zircon ages (Wang et al., 2013 Precam. Res., 231: 343-371) | amphibolites and metagabbro | amphibolite | intra-oceanic arc to back arc | X | X | X | Y | |||||||||||||
51 | Dunzhugur ophiolite | Russia | Central Asian Orogenic Belt | 1020 | 10 | multigrain zircon 207Pb/206Pb age (Khain et al., 2002 EPSL, 199: 311-325) | tholeiitic dykes and lavas, boninitic lavas | forearc | X | X | X | X | Y | |||||||||||||
52 | Miaowan ophiolite | China | Yangtze craton | 1042.5 | 57.5 | average of range of ages (Peng et al., 2012 Gond. Res., 21: 577-594) | pillow lavas, isotropic and layered metagabbro, diabase dikes | greenschist | forearc | X | ~X | Y | ||||||||||||||
53 | Areachap Group | South Africa | Namaqua Mobile Belt | 1241 | 12 | SHRIMP U-Pb zircon (Pettersson et al., 2007, PR, 158:79-92) | amphibolites (metabasalts) | amphibolite | intra-oceanic arc | X | X | X | Y | Y | ||||||||||||
54 | Tudor and Kashwakamak Formations | Ontario, Canada | Grenville Province | 1279 | 3 | U-Pb zircon (Heaman et al., 1987) | tholeiitic basalts, basaltic andesites, and andesites (pillowed flows, cut by basaltic dikes and sills) | upper greenschist to lower amphibolite | intra-oceanic arc | X | Y | |||||||||||||||
55 | Fisher Massif | Pricnce Charles Mountains, Eastern Antarctica | 1300 | 4 | TIMS U-Pb zircon age (upper intercept concordia of multiple samples, Beliatsky et al. 1994) | basalts (basaltic andesites, dacites, rhyodacites, and rhyolites also present in Massif) | lower amphibolite | intra-oceanic arc | X | X | Y | Y | ||||||||||||||
56 | Coal Creek Domain | Texas, USA | Llano uplift | 1305 | 25 | reported age range from Furnes et al., 2015 Gond. Res., 27: 649-685. | metabasalt, metagabbro | amphibolite | intra-oceanic arc | ~X | X | Y | ||||||||||||||
57 | Trincheira Complex | Brazil | Amazon craton | 1335 | 15 | reproted age range from Rizzotto and Hartmann, 2012 Lithos, 148: 277-295 | amphibolites | amphibolite | intra-oceanic arc | ~X | X | Y | ||||||||||||||
58 | Payson ophiolite | Arizona, USA | Yavapai-Mazatzal | 1729 | 6 | TIMS U-Pb zircon age (Dann, 1997 GSAB, 109: 347-365) | sheeted dikes, diorites, gabbros, and tonalite | greenschist | intra-oceanic-arc rifting | X | X | X | Y | |||||||||||||
59 | Green Mountain paleo-arc | Wyoming, USA | 1782 | 7 | U-Pb zircon age from metagabbro (Jones et al., 2010 GSA Bul., 122: 1877-1898) | gabbro, granodiorite | upper amphibolite | intra-oceanic arc | X | X | X | Y | ||||||||||||||
60 | Pembine-Wausau terrane | Wisconsin, USA | Penokean orogen | 1842 | 4 | bracket of U-Pb zircon ages for syntectonic granodiorites (Sims et al., 1993 USGS Bulletin, 1904-j) | orthogneiss, tonalite, quartz diorite, granodiorite | greenschist | intra-oceanic arc | X | X | X | Y | |||||||||||||
61 | Flin Flon–Snow Lake Greenstone Belt | Saskatchewan/Manitoba, Canada | Flin-Flon belt, Trans-Hudson orogen | 1888 | 1 | ID-TIMS U-Pb zircon from Cliff Lake pluton quartz diorite (Rayner, 2010 Geol. Surv. Can., Current Research 2010-4, p. 12) | basalt, basaltic-andesites, andesits, and boninites | upper greenschist to lower amphibolite | intra-oceanic arc | X | X | X | X | Y | ||||||||||||
62 | Skellefte district | Sweden | Svecofennian orogen | 1890 | 8 | U-Pb zircon age on granitoid of the Jörn group which are consider to have been comagmatic with the volcanics (Wilson et al., 1987, Precamb. Res. 36: 201-225.) | basalts to dacites | upper greenschist to lower amphibolite | intra-oceanic arc | X | X | X | Y | Y | ||||||||||||
63 | Birmian greenstone belt | West Africa | West African craton | 2100 | 100 | see age range given based on existing U-Pb zircon geochronology (Sylvester and Attoh, 1992, J. of Geol. 100: 377-393). | plutonic rocks (gabbro, diorite, granite) and volcanic rocks (basalt, andesite, and rhyolite) | greenschist | intra-oceanic arc | ~X | X | Y | Y | |||||||||||||
64 | Nuttio ophiolite | Finland | 2100 | 100 | whole rock Sm-Nd isochron age, poor age control, 100 myr error is arbitrary (Hanski and Huhma, 2005 Dev. Prec. Geol., 14: 139-193) | basaltic dikes | - | intra-oceanic arc | X | X | Y | |||||||||||||||
65 | Wutaishan greenstone belt | China | North China craton | 2523 | 3 | U-Pb SHRIMP zircon age, (Wang et al., 2004 Precam. Res., 131: 323-343) | amphibolite, basalts, and andesites | greenschist to amphibolite | intra-oceanic arc | X | X | X | Y | |||||||||||||
66 | Zanhuang complex | China | North China craton | 2540 | 23 | Pb-Pb zircon age from granite cross-cutting mélange, exact formation age of blocks in mélange and cross-cutting dikes unknown (Deng et al., 2013 Lithos, 175: 193-212) | basaltic blocks in melange and mafic dikes | amphibolite | intra-oceanic arc | X | Y | |||||||||||||||
67 | Hutti greenstone belt | India | Dharwar craton | 2586 | 50 | U-Pb zircon age on felsic rocks from the greenstone belt (Buddine Formation) (Rogerst et al., 2007, J. Asian Earth Sci. 31, 55–70.) | basalts and andesites | upper greenschist to lower amphibolite | intra-oceanic arc | X | Y | |||||||||||||||
68 | Wawa greenstone belt | Canada | Superior craton | 2685 | 35 | summarized age range in Polat and Kerrich, 2000 EPSL, 175: 41-54. | basalts (arc-related only) | greenschist to amphibolite | intra-oceanic arc | X | Y | |||||||||||||||
69 | Confederation assemblage, Birch-Uchi Greenstone belt | Canada | Superior craton | 2737 | 2 | Average of U-Pb zircon ages for felsic sequences in Confederation assemblage (Nunes and Thurston, 1980, Can. J. of Earth Sci. 23: 251-285. Noble, 1989, PhD Thesis, Univ. of Toronto) | basalts to felsic volcanics | amphibolite | intra-oceanic arc | ~X | X | Y | ||||||||||||||
70 | Lake of the Woods greenstone belt | Canada | Wabigoon subprovince, Superior craton | 2738 | 2 | U-Pb zircon age from oldest volcanic unit (Ayer and Davis, 1997, Precamb. Res. 81: 155-178) | mostly mafic flows, one intermediate flow | - | intra-oceanic arc to back arc basin | ~X | X | X | Y | |||||||||||||
71 | Kushtagi-Hungund-Ramagiri greenstone belt | India | Dharwar craton | 2746 | 64 | Pb-Pb zircon age (Zachariah et al., 1995, Zachariah et al., 1997 Cont. Min. Petr., 129: 87-104) | basalts | amphibolite | intra-oceanic arc | X | Y | |||||||||||||||
72 | Kalikorva structure | Russia | Baltic shield | 2785 | 13 | SHRIMP U-Pb zircon age from metadacite of upper sequence volcanics (Mil'Kevich et al. | basalts to dacites | amphibolite | intra-oceanic arc to back arc basin | X | Y | |||||||||||||||
73 | Storø greenstone belt | SW Greenland | 2800 | 50 | poor age control, best estimate of age range given in Ordóñez-Calderón et al. 2011 Precam. Res., 184: 24-42. | amphibolites | amphibolite | arc | X | Y | ||||||||||||||||
74 | Fiskenæsset complex | SW Greenland | 2973 | 28 | Sm-Nd whole rock age (Polat et al., 2010 Geology, 277: 1-20) | basalts | amphibolite | intra-oceanic arc | X | Y | ||||||||||||||||
75 | Ivisaartoq and Ujarassuit greenstone belts | SW Greenland | 3075 | 15 | U-Pb zircon age (Friend and Nutman, 2005 J. Geol Soc., 162: 147-162) | amphibolites | amphibolite | intra-oceanic arc | X | Y | ||||||||||||||||
76 | Whundo Group | Australia | Pilbara craton | 3120 | 5 | Compliation of U-Pb zircon SHRIMP ages from the W. Aust. Geol. Surv (Smithies et al., 2005 EPSL, 231: 221-237) | basalts to rhyolites, boninites | greenschist | intra-oceanic arc | X | X | X | X | Y | ||||||||||||
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96 | ||||||||||||||||||||||||||
97 | ||||||||||||||||||||||||||
98 | ||||||||||||||||||||||||||
99 | ||||||||||||||||||||||||||
100 | ||||||||||||||||||||||||||