Updated LIP Record Through Time and Postulated Links with Significant Environmental Changes and Geological Time-Scale Boundaries
Richard E. Ernst
Department of Earth Sciences, Carleton University, Ottawa, Canada &
Faculty of Geology and Geography, Tomsk State University, Russia
Email: Richard.Ernst@ErnstGeosciences.com
Here is an updated compilation of the global LIPs record and links with environmental changes and geological time scale boundaries. The attached Table and Figure are extracted and slightly modified from Chapter 1 of a new AGU book GM 255 “Large Igneous Provinces: A Driver of Global Environmental and Biotic Changes”
https://agupubs.onlinelibrary.wiley.com/doi/book/10.1002/9781119507444 is Open Access for free download. See also the January 2021 LIP of the Month for http://www.largeigneousprovinces.org/21jan for an overview of the 21 chapters in the book.
For more details on the events (including referencing) see the published Chapter 1 https://agupubs.onlinelibrary.wiley.com/doi/10.1002/9781119507444.ch1
The full reference for Chapter 1 is:
Ernst, R.E., Bond, D.P.G., Zhang, S-H., Buchan, K.L., Grasby, S.E., Youbi, N., El Bilali, H., Bekker, A. & Doucet, L. (2021). Large Igneous Province Record Through Time and Implications for Secular Environmental Changes and Geological Time-Scale Boundaries. Chapter 1 In: Ernst, R.E., Dickson, A.J., Bekker, A. (eds.) Large Igneous Provinces: A Driver of Global Environmental and Biotic Changes. AGU Geophysical Monograph 255, pp. 3-26.
Included in this compilation are LIPs that satisfy the definition of
“Large igneous provinces are voluminous (> 0.1 Mkm3 ( = 106 km3); frequently above 1 Mkm3), mainly mafic (ultramafic) magmatic events of intraplate affinity (based on tectonic setting and/or geochemistry) that occur in both continental and oceanic settings, are often linked with mantle plumes, and are typically emplaced over a short time period ( < 5 myr; often < 2 myr) or in multiple short pulses with a maximum duration of a few tens of myrs”. Also catalogued are intraplate events of smaller size which are interpreted as LIPs (LIP ‘fragments/remnants’) that have been reduced in size by plate tectonic fragmentation and/or erosion. Continental, oceanic and accreted oceanic LIPs are distinguished and Silicic LIPs (SLIPs) are also included.
Figure 1: Global maps (a–f) showing the schematic distribution of LIPs (including interpreted LIP ‘fragments’) and SLIPs through time. Abbreviations: CAMP = Central Atlantic Magmatic Province; HALIP = High Arctic Large Igneous Province; NAIP -= North Atlantic Igneous Province; OJP Ontong Java plateau. BRIC = Booth River intrusive complex. CSDG = Central Scandinavian Dolerite Complex. Maps are in Robinson projection. Continental LIPs are in black, oceanic LIPs are in blue, accreted oceanic LIPs are in purple, and silicic LIPs are in orange. Numbers are ages in Ga. Table 1 provides additional information on each event.
Table 1:LIPs Through Time and Matches (Definite and Approximate) With the GTS (Geological Time-Scale) Boundaries and Potential Environmental Changes. For referencing see https://agupubs.onlinelibrary.wiley.com/doi/10.1002/9781119507444.ch1
LIP type |
LIP |
Location |
Age (Ma) |
Area (106 km2) |
Age (numeric) |
Area (numeric) |
LIP-type (numeric) |
Chronostratigraphic boundary &/or environmental change (timing in Ma) |
C |
Columbia River |
w North America |
16.7-15.9 |
0.67 |
16 |
0.67 |
1 |
End Burdigalian 15.97; mid-Miocene Climate Optimum 16 |
C |
Afro-Arabian |
East Africa, Arabian Peninsula |
main 31 (precursor 34) |
2.4 |
31 |
2.4 |
1 |
Middle Rupelian (end Priabonian) |
S |
Sierra Madre Occidental |
sw North America |
38-18 |
0.40-1.00 |
38 |
1 |
3 |
End Bartonian 38.00 |
Oa |
Siletzia (Crescent, Prometheus, Yakutat) |
w North America |
56-49 |
0.04 |
56 |
0.04 |
2 |
End Thanetian 56.0, PETM 56 |
O |
Benham Rise |
Philippine Sea |
48-41 |
0.11 |
48 |
0.11 |
2 |
|
C |
NAIP (North Atlantic Igneous Province) |
Europe & Greenland |
62 & 55 Ma |
1.1 |
62 |
1.1 |
1 |
62 pulse: End Danian 61.6 or end Selandian 59.2; 55 pulse: End Thanetian 56.0, PETM 56 |
C |
Deccan |
India+ Chagos-Laccadive & Seychelles portions |
66 |
1.85 |
66 |
1.85 |
1 |
End Cretaceous 66.0 (Schoene et al., 2019); mass extinction; also bolide link |
O |
Maud Rise |
s Atlantic ocean |
ca. 70 |
0.07 |
70 |
0.07 |
2 |
End Campanian 72.1 |
O |
Sierra Leone Rise |
Atlantic ocean |
ca. 70 |
0.27 |
70 |
0.27 |
2 |
End Campanian 72.1 |
O |
Crozet |
Indian ocean |
70-74 |
---- |
74 |
-9999 |
2 |
End Campanian 72.1 |
O |
Conrad Rise |
Indian ocean |
73 |
---- |
73 |
-9999 |
2 |
|
C |
Madagascar |
Madagascar |
89 |
0.61 |
89 |
0.61 |
1 |
End Turonian 89.8, |
O |
Del Cano |
Indian ocean |
90 |
90 |
-9999 |
2 |
End Turonian 89.8, |
|
O, Oa |
Caribbean-Colombian |
Caribbean |
90- 87 |
1.54 |
90 |
1.54 |
2 |
End Cenomanian 93.9 |
C |
Hess Rise |
Pacific ocean |
ca. 100 |
0.14 |
100 |
0.14 |
1 |
End Albian 100.5 |
C |
Naturaliste Plateau |
Indian ocean |
ca. 100 |
0.03 |
100 |
0.03 |
1 |
End Albian 100.5 |
Oa |
Malaita & Bohol |
Indonesia |
120 & 100 |
---- |
120 |
-9999 |
2 |
|
Oa |
possible Hawaii starting plume LIP |
Kamchatka-Okhotsk region |
c. 100 |
---- |
100 |
-9999 |
2 |
|
O |
Southwest African (Agulhas) |
off s Africa |
120-100 |
0.5 |
120 |
0.5 |
2 |
|
S |
Whitsunday |
e Australia |
120-90 |
>0.4 |
120 |
0.4 |
3 |
|
O, Oa |
Ontong Java Nui (Greater Ontong Java, Manihiki, Hikurangi OPs + Sorachi-Yezo, Pinon accreted OPs) |
s Pacific |
ca. 120 |
6.41 |
120 |
6.41 |
2 |
Mid Aptian, Selli Anoxia ~120 |
O |
Wallaby (Cuvier) Plateau |
off nw Australia |
ca. 120 |
0.05 |
120 |
0.05 |
2 |
Mid Aptian, Selli Anoxia ~120 |
C,O |
HALIP (High Arctic) |
North America, Asia, Europe, Alpha-Mendeleev rise |
126-121 & 95 |
7.4 |
126 |
7.4 |
1 |
End Barremian 126.3 (end Cenomanian 93.9) |
Oa |
Central Tibetan Meso-Tethyan-2 (Zhongba, Saga-sangsang |
Tibet |
128–104 Ma |
0.2 |
128 |
0.2 |
2 |
End Barremian 126.3 (end Cenomanian 93.9) |
C,O |
Bunbury-Comei + Kerguelen - Rajmahal |
Indian Ocean, India |
134 & 110 / 86 |
1.6 |
134 |
1.6 |
1 |
134 pulse: End Valanginian 134.7, Valanginian-Weissert; C-isotope excursion 135.2 |
O |
Mid-Pacific Mountains |
Pacific ocean |
ca. 130 |
0.59 |
130 |
0.59 |
2 |
134 pulse: End Valanginian 134.7, Valanginian-Weissert; C-isotope excursion 135.2 |
C |
EQUAMP (Equatorial Atlantic Magmatic Province) |
ne South America |
ca. 135 |
0.65 |
135 |
0.65 |
1 |
134 pulse: End Valanginian 134.7, Valanginian-Weissert; C-isotope excursion 135.2 |
C |
Parana-Etendeka (includes rifted margin magmatism) |
South America, Africa |
134 |
3.47 |
134 |
3.47 |
1 |
134 pulse: End Valanginian 134.7, Valanginian-Weissert; C-isotope excursion 135.2 |
C |
Trap |
sw Greenland |
ca. 140 |
0.03 |
140 |
0.03 |
1 |
|
Oa East Sulawesi |
East Sulawesi |
Indonesia |
138 & 80 ? |
---- |
138 |
-9999 |
2 |
|
C |
Magellan Rise |
Pacific ocean |
ca. 150 |
0.03 |
150 |
0.03 |
1 |
End Kimmeridgian 152.1 |
Oa |
Sanbagawa |
Paleo-Pacific Ocean |
Ca. 150 |
---- |
150 |
-9999 |
2 |
End Kimmeridgian 152.1 |
O |
Shatsky Rise-Tamu |
Pacific ocean |
ca. 150 |
0.42 |
150 |
0.42 |
2 |
End Kimmeridgian 152.1 |
C |
NW Australian Margin |
off nw Australia |
160-140 |
2.12 |
160 |
2.12 |
1 |
|
Oa |
Lesser Caucasus |
Caucasus |
168-160 |
---- |
168 |
-9999 |
2 |
Middle-late Jurassic (163.1) |
C |
Karoo |
s Africa, Antarctica |
183.25 |
3.15 |
183 |
3.15 |
1 |
End Pliensbachian 183.7; link with early Toarcian Oceanic Anoxic Event |
C |
Ferrar |
Antarctica, Tasmania |
182.8 |
0.18 |
183 |
0.18 |
1 |
End Pliensbachian 183.7; link with early Toarcian Oceanic Anoxic Event |
S |
Chon Aike |
South America |
1st pulse 180 |
---- |
183 |
-9999 |
3 |
End Pliensbachian 183.7; link with early Toarcian Oceanic Anoxic Event |
Oa |
Central Tibetan Meso-Tethyan-1 |
Tibet |
193-172 |
0.2 |
193 |
0.2 |
2 |
|
C |
CAMP (Central Atlantic Magmatic Province) |
North America, Europe, Africa, South America |
201 |
11.28 |
201 |
11.28 |
1 |
End Triassic 201.4; mass extinction |
Oa |
Wrangellia (North & South portions) |
w North America |
232 |
0.16 |
232 |
0.16 |
2 |
Late Carnian (End Carnian ~227); Carnian Pluvial Event (or HuMid Episode) and minor extinctions |
Oa, C |
Angayucham (Wrangellia?) |
nw North America |
230 ? |
0.1 |
230 |
0.1 |
2 |
Late Carnian (End Carnian ~227); Carnian Pluvial Event (or HuMid Episode) and minor extinctions |
C |
Siberian Traps |
n Siberia |
252.27-251.354 |
3.47 |
252 |
3.47 |
1 |
End Permian 251.9; mass extinction |
C |
Emeishan |
s China |
259.6-257.6 |
0.7 |
259 |
0.7 |
1 |
End Capitanian 259.8, P3-P4 glaciation 273–260 |
S |
Choiyoi |
South America |
ca. 265 |
1.68 |
265 |
1.68 |
3 |
GSSP Marker |
C |
Himalaya Neotethys (main, + Abor & Woniusi portions) |
See Panjal – South Qiangtang on Fig. 1 |
ca. 280 |
0.14 |
280 |
0.14 |
1 |
End Sakmarian 290.1, P2 glaciation 287–280 |
C |
Panjal |
Himalaya |
289 |
0.04 |
289 |
0.04 |
1 |
End Sakmarian 290.1, P2 glaciation 287–280 |
C |
South Qiangtang |
Central Asia |
ca. 280 |
0.07 |
280 |
0.07 |
1 |
End Sakmarian 290.1, P2 glaciation 287–280 |
C |
Tarim |
Central Asia |
ca. 290-280 |
0.25 |
290 |
0.25 |
1 |
End Sakmarian 290.1, P2 glaciation 287–280 |
C |
Skagerrak (Skagerrak centered; Jutland) |
Scandinavia |
300 |
0.8 |
300 |
0.8 |
1 |
End Gzhelian 298.9, P1 glaciation 300–290 |
S |
Barguzin-Vitam |
Central Asia |
ca. 300 |
0.15 |
300 |
0.15 |
3 |
End Gzhelian 298.9, P1 glaciation 300–290 |
S |
Kennedy-Conners |
e. Australia |
320-280 |
---- |
320 |
-9999 |
3 |
|
Oa |
Mino-Tamba belt |
e. Asia |
340-330 |
---- |
340 |
-9999 |
2 |
|
C |
Kola-Dnieper |
East European craton |
ca. 375, 365 |
2.96 |
375 |
2.96 |
1 |
End Frasnian; middle Famennian, end Graptolites; Frasnian-Famennian, and the Devonian-Carboniferous boundary (Hangenberg Event) |
C |
Yakutsk-Vilyui |
Siberia |
ca. 375, 365 |
1.15 |
375 |
1.15 |
1 |
End Frasnian; middle Famennian, end Graptolites; Frasnian-Famennian, and the Devonian-Carboniferous boundary (Hangenberg Event) |
C |
Altay-Sayan |
c Asia |
ca. 420-390 |
0.35 |
400 |
0.35 |
1 |
End Silurian 419.2 or Eifelian 393.3–387.7 |
C |
Suordakh |
e Siberia |
ca. 440 |
0.4 |
440 |
0.4 |
1 |
End Katian 445.2 or end Hirnantian 443.8, Hirnantian glaciation 440 |
C |
Kalkarindji |
Australian craton |
510 |
3.51 |
510 |
3.51 |
1 |
End Age 4 (Epoch 2) 509, ROECE anomaly |
C |
Wichita |
sw Laurentia |
533 |
0.18 |
533 |
0.18 |
1 |
End Fortunian ca. 530 |
C |
Paraupebas-Piranhas |
Amazonian craton |
535 |
---- |
535 |
-9999 |
1 |
End Fortunian ca. 530 |
Oa |
Precordillera |
South America |
576 |
----- |
576 |
-9999 |
2 |
Mid Ediacaran, Gaskier glaciation 580 |
C |
CIMP-Ouarzazate |
West African craton |
580-560 |
0.06 |
580 |
0.06 |
1 |
Mid Ediacaran, Gaskier glaciation 580 |
C |
CIMP Volyn, Seiland |
Baltica |
ca. 580-570 |
0.16 |
580 |
0.16 |
1 |
Mid Ediacaran, Gaskier glaciation 580 |
C |
CIMP 590-560 Ma pulse (Grenville dykes) |
e Laurentia |
ca. 580 |
0.36 |
580 |
0.36 |
1 |
Mid Ediacaran, Gaskier glaciation 580 |
C |
Baltoscandian - Egersund |
Baltica |
615 |
0.07 |
615 |
0.07 |
1 |
Early Ediacaran |
C |
CIMP - 615 Ma pulse (Long Range pulse) |
e Laurentia |
615 |
0.1 |
615 |
0.1 |
1 |
Early Ediacaran |
C |
Franklin (-Thule) |
Canada & Greenland portions, n. Laurentia |
716.5 |
2.64 |
720 |
2.64 |
1 |
End Tonian 716.5 (start Sturtian glaciation) |
C |
Kikitat |
Alaska |
715 |
---- |
715 |
-9999 |
1 |
End Tonian 716.5 (start Sturtian glaciation) |
C |
Irkutsk |
Siberia craton |
720 |
0.3 |
720 |
0.3 |
1 |
End Tonian 716.5 (start Sturtian glaciation) |
C |
Mutare-Fingeren |
Kalahari & Grunehogna cratons |
720 |
0.05 |
720 |
0.05 |
1 |
End Tonian 716.5 (start Sturtian glaciation) |
C,S |
Malani |
India, Seychelles, greater Indian craton |
755 |
0.02 |
755 |
0.02 |
3 |
Late Tonian |
C |
Mount Rogers |
e Laurentia |
ca. 760-740 |
0.06 |
760 |
0.06 |
1 |
Late Tonian |
C |
Mundine Well-Keene |
West Australian craton |
755-750 |
0.38-0.65 |
755 |
0.65 |
1 |
Late Tonian |
C |
Ogcheon |
North China craton |
755 |
0.02 |
755 |
0.02 |
1 |
Late Tonian |
C |
Seychelles |
Seychelles |
755 |
0.01 |
755 |
0.01 |
1 |
Late Tonian |
C,S |
Shaba |
South China block |
755 |
0.3 |
755 |
0.3 |
3 |
Late Tonian |
C |
Roan |
Congo craton |
765-735 |
---- |
765 |
-9999 |
1 |
Late Tonian |
C |
Boucaut |
s West Australian craton |
780 |
0.01 |
780 |
0.01 |
1 |
Late Tonian |
C |
Gunbarrel |
w Laurentia (north & south portions) |
780 |
0.83 |
780 |
0.83 |
1 |
Late Tonian |
C,S |
Kanding |
South China block |
780 |
1.16 |
780 |
1.16 |
3 |
Late Tonian |
C,S |
Kudi |
Tarim block |
780 |
1.16 |
780 |
1.16 |
3 |
Late Tonian |
C |
Gannakouriep |
sw Kalahari craton |
800 |
0.02 |
800 |
0.02 |
1 |
Mid Tonian |
C |
Niquelândia |
Brasilia belt |
790 |
---- |
790 |
-9999 |
1 |
Mid Tonian |
C |
Rushinga-Bukoba |
s Africa |
Ca. 800 |
---- |
800 |
-9999 |
1 |
Mid Tonian |
C,S |
Suxiong-Xiaofeng |
South China block |
800 |
---- |
800 |
-9999 |
3 |
Mid Tonian |
C |
Gairdner-Willouran |
s Australian craton |
825 |
1.32 |
825 |
1.32 |
1 |
Mid Tonian ca. 15 myr older than Bitter Springs anomaly) |
C,S |
Guibei |
South China block |
825 |
1.33 |
825 |
1.33 |
3 |
Mid Tonian ca. 15 myr older than Bitter Springs anomaly) |
C |
Kuluketage (Qiganbualke) |
Tarim block |
---- |
825 |
-9999 |
1 |
Mid Tonian |
|
Oa |
Arabian-Nubian |
Arabian–Nubian Shield |
ca. 850 |
---- |
850 |
-9999 |
2 |
Mid Tonian |
C |
Zambezi (Munali) |
Zambia, Congo craton |
880-860 |
---- |
870 |
-9999 |
1 |
Mid Tonian |
C |
Manso |
n West African craton |
ca. 880 |
---- |
880 |
-9999 |
1 |
Mid Tonian |
C |
Iguerda-Taifast |
s West African craton |
ca. 870 |
---- |
870 |
-9999 |
1 |
Mid Tonian |
C |
Sailajiazitage |
Tarim craton |
890 |
---- |
890 |
-9999 |
1 |
Mid Tonian |
C |
Dashigou (Sariwon) |
North China craton |
920 |
0.5 |
920 |
0.5 |
1 |
Mid Tonian, (?) black shale (anoxia event) ca. 920 |
C |
Bahia - Araquai |
Sao Francisco craton |
920 |
0.15 |
920 |
0.15 |
1 |
Mid Tonian, (?) black shale (anoxia event) ca. 920 |
C |
Zadinian-Mayumbian |
Greater Congo craton |
924-912 |
0.34 |
924 |
0.34 |
1 |
Mid Tonian, (?) black shale (anoxia event) ca. 920 |
C |
Sette-Daban |
e Siberian craton |
1005, 975 |
0.05 |
1005 |
0.05 |
1 |
End Stenian 1000 |
C |
Warakurna |
c Australian craton |
1075 |
1.56 |
1075 |
1.56 |
1 |
Mid Stenian |
C |
Southwest Laurentia (formerly Southwest Diabase Province) |
sw Laurentia |
1100-1070 |
1.08 |
1090 |
1.08 |
1 |
Mid Stenian |
C |
Keweenawan (Mid-Continent rift event) |
c Laurentia |
1115-1085 |
0.47 |
1115 |
0.47 |
1 |
Mid Stenian, (?)black shale (anoxia event) ca. 1100 |
C |
Huila (GN) - Epembe |
sw Congo craton |
1110 |
0.03 |
1110 |
0.03 |
1 |
Mid Stenian, (?)black shale (anoxia event) ca. 1100 |
C |
Mahoba |
Bundelkhand craton |
1110 |
0.01 |
1110 |
0.01 |
1 |
Mid Stenian, (?)black shale (anoxia event) ca. 1100 |
C |
Huanchaca - Rincon del Tigre |
Amazonia |
1110 |
0.21 |
1110 |
0.21 |
1 |
Mid Stenian, (?)black shale (anoxia event) ca. 1100 |
C |
Umkondo (Africa) |
Kalahari craton |
1112-1106 |
2 |
1112 |
2 |
1 |
Mid Stenian, (?)black shale (anoxia event) ca. 1100 |
C |
Umkondo (Antarctica) |
Grunehogna craton |
1112-1106 |
0.22 |
1112 |
0.22 |
1 |
Mid Stenian, (?)black shale (anoxia event) ca. 1100 |
C |
Bunger Hills |
Antarctica |
1130 |
--- |
1130 |
-9999 |
1 |
Mid Stenian |
C |
Abitibi [dykes]- Corson |
c. Laurentia |
1140-1150 |
0.31 |
1145 |
0.31 |
1 |
Early Stenian |
C |
Thiselthwaite-Munn |
nw Laurentia |
1170 |
---- |
1170 |
-9999 |
1 |
Early Stenian |
C |
Marnda Moorn |
Yilgarn craton |
1210 |
0.71 |
1210 |
0.71 |
1 |
End Ectasian 1200 |
C |
Licheng-Yishui (1230, 1210 Ma) |
North China craton |
1230-1210 |
0.05 |
1230 |
0.05 |
1 |
End Ectasian 1200 |
C |
Nova Floresta |
Amazonian |
1220 |
---- |
1220 |
-9999 |
End Ectasian 1200 |
|
C |
Sudbury [dykes] |
e Laurentia |
1235 – 1238 |
0.18 |
1235 |
0.18 |
1 |
Late Ectasian |
C |
Vestfold Hills-5 |
Antarctica |
1240 |
---- |
1240 |
-9999 |
1 |
Late Ectasian |
C |
Mealy-Seal Lake |
e Laurentia |
1250 |
0.02 |
1250 |
0.02 |
1 |
Mid Ectasian |
C |
CSDG (Central Scandinavian Dolerite Complex) |
Baltica |
1270-1250 |
0.27 |
1270 |
0.27 |
1 |
Mid Ectasian |
C |
Srednecheremshanskii |
Siberian craton |
1260 |
---- |
1260 |
-9999 |
1 |
Mid Ectasian |
C |
Harp |
Nain portion, North Atlantic craton |
1270 |
0.07 |
1270 |
0.07 |
1 |
Mid Ectasian |
C |
Mackenzie |
Laurentia |
1272-1265 |
2.9 |
1272 |
2.9 |
1 |
Mid Ectasian |
C |
Juscelândia-Serra dos Borges |
Brasilia belt |
ca. 1300-1250 |
---- |
1270 |
-9999 |
1 |
Mid Ectasian |
C |
Galiwinku - Derim Derim |
North Australian craton |
1320 |
0.19 |
1320 |
0.19 |
1 |
Mid Ectasian |
C |
Yanliao |
North China craton |
1320 |
0.08 |
1320 |
0.08 |
1 |
Mid Ectasian |
C |
Hart River - Salmon River Arch |
w Laurentia |
1380 |
0.02 |
1380 |
0.02 |
1 |
End Calymmian 1400 (1385), (?) black shale (anoxia event) 1385 |
C |
Vestfold Hills-4 |
Antarctica |
1380 |
---- |
1380 |
-9999 |
1 |
End Calymmian 1400 (1385), (?) black shale (anoxia event) 1385 |
C |
Chieress (Severobyrrang) |
n Siberian craton |
1384 (1360) |
0.02 |
1384 |
0.02 |
1 |
End Calymmian 1400 (1385), (?) black shale (anoxia event) 1385 |
C |
Kunene-Kibaran |
Greater Congo craton |
1380-1360 |
2.1 |
1380 |
2.1 |
1 |
End Calymmian 1400 (1385), (?) black shale (anoxia event) 1385 |
C |
Mashak |
e Baltica |
1385 |
0.09 |
1385 |
0.09 |
1 |
End Calymmian 1400 (1385), (?) black shale (anoxia event) 1385 |
C |
Midsommerso - Zig Zag Dal |
Greenland, ne Laurentia |
1385 |
0.1 |
1385 |
0.1 |
1 |
End Calymmian 1400 (1385), (?) black shale (anoxia event) 1385 |
C |
Biberkine |
Yilgarn craton |
1390 |
---- |
1390 |
-9999 |
1 |
End Calymmian 1400 (1385), (?) black shale (anoxia event) 1385 |
C |
Bas Draa |
Anti Atlas inliers, West African craton |
1415-1380 |
---- |
1415 |
-9999 |
1 |
Late Calymmian |
C |
Salto do Céu – Figuera Branca – Nova Lacerda |
Amazonia |
1440–1420 & 1380 |
---- |
1430 |
-9999 |
1 |
Late Calymmian |
C |
Lakhna & Bandlimal |
Bastar craton |
1440 |
0.04 |
1440 |
0.04 |
1 |
Late Calymmian |
C |
Betara |
Betara block |
1445 |
0.09 |
1445 |
0.09 |
1 |
Late Calymmian |
C |
Michael - Shabagamo |
e Laurentia |
ca. 1430 |
0.07 |
1430 |
0.07 |
1 |
Late Calymmian |
C |
Moyie |
w Laurentia |
1460 |
0.11 |
1460 |
0.11 |
1 |
Late Calymmian |
C |
Tuna-Trond Gota-Lake Ladoga |
n Baltica |
1460-1450 |
0.68 |
1460 |
0.68 |
1 |
Late Calymmian |
C |
Bangemall |
nw Australian craton |
1465 |
0.04 |
1465 |
0.04 |
1 |
Late Calymmian |
C |
Curaca- Chapada Diamantina |
Sao Francisco craton |
1500 |
0.18 |
1500 |
0.18 |
1 |
Mid Calymmian, (?)black shales (anoxia event) ca. 1500 |
C |
Humpata |
Greater Congo craton |
1500 |
---- |
1500 |
-9999 |
1 |
Mid Calymmian, (?)black shales (anoxia event) ca. 1500 |
C |
Kuonamka |
n Siberian craton |
1500 |
0.07 |
1500 |
0.07 |
1 |
Mid Calymmian, (?)black shales (anoxia event) ca. 1500 |
C |
Essakane |
Amazonia |
1520 |
0.5 |
1520 |
0.5 |
1 |
Mid Calymmian |
C |
Kayser |
West African craton |
1520 |
--- |
1520 |
-9999 |
1 |
Mid Calymmian |
C |
Korsimoro |
West African craton |
1575 |
0.16 |
1575 |
0.16 |
1 |
Early Calymmian |
C |
Mata Mata |
Amazonia |
1575 |
---- |
1575 |
-9999 |
1 |
Early Calymmian |
C,S |
Gawler Range |
Gawler-Curnamona craton |
1590 |
0.57 |
1590 |
0.57 |
3 |
End Statherian 1600 |
C |
Mammoth-Western Channel |
w. Laurentia |
1590 |
0.32 |
1590 |
0.32 |
1 |
End Statherian 1600 |
C |
Tandil |
Rio de la Plata craton |
1590 |
---- |
1590 |
-9999 |
1 |
End Statherian 1600 |
C |
Breven-Hallefors |
Baltica |
1600 |
0.06 |
1600 |
0.06 |
1 |
End Statherian 1600 |
C |
Taishan |
North China craton |
1630-1620 |
0.05 |
1630 |
0.05 |
1 |
Late Statherian, (?)black shales (anoxia event) ca. 1650 |
C |
Melville Bugt (Greenland) |
ne Laurentia |
1640-1630 |
0.12 |
1640 |
0.12 |
1 |
Late Statherian, (?)black shales (anoxia event) ca. 1650 |
C |
Zenaga |
Anti Atlas inliers, West African craton |
1660 |
0.01 |
1660 |
0.01 |
1 |
Mid Statherian |
C |
Hame |
Baltica |
1676-1640 |
0.01 |
1676 |
0.01 |
1 |
Mid Statherian |
C |
Laiwu |
North China craton |
1670 |
0.01 |
1670 |
0.01 |
1 |
Mid Statherian |
C |
Toole Creek (Dead Horse, Cobbold) & Bulonga |
North Australian craton |
1660-1670 |
---- |
1670 |
-9999 |
1 |
Mid Statherian |
C |
Late Calvert (Sybella) (Willyama?) |
North Australian craton |
1690-1670 |
---- |
1680 |
-9999 |
1 |
Mid Statherian |
C |
Pelly Bay |
n Laurentia |
1700 |
0.02 |
1700 |
0.02 |
1 |
Mid Statherian |
C |
Fiery Creek (Oenpelli?) |
North Australian craton |
1730-1710 |
---- |
1720 |
-9999 |
1 |
Mid Statherian |
C |
Wonga |
North Australian craton |
1740 |
---- |
1740 |
-9999 |
1 |
Mid Statherian |
C |
Miyun, Damiao-Shachang |
North China craton |
1730-1680 |
0.09 |
1730 |
0.09 |
1 |
Mid Statherian |
C |
Kivalliq (Pitz-Nueltin, McRae, Wellington, Cleaver portions) |
n Laurentia |
1770-1730 (peak 1750) |
0.09 |
1750 |
0.09 |
1 |
Statherian, (?) black shales (anoxia event) ca. 1750 |
C |
Aiskii (Navysh) |
e Baltica |
1750 |
---- |
1750 |
-9999 |
1 |
Statherian, (?) black shales (anoxia event) ca. 1750 |
C |
Lunch Creek (north & south) / Mt. Isa |
North Australian craton |
1750 |
0.13 |
1750 |
0.13 |
1 |
Statherian, (?) black shales (anoxia event) ca. 1750 |
C |
Timpton |
Siberian craton |
1750 |
0.42 |
1750 |
0.42 |
1 |
Statherian, (?) black shales (anoxia event) ca. 1750 |
C |
Vestfold Hills-3 |
Antarctica |
ca. 1750 |
---- |
1750 |
-9999 |
1 |
Statherian, (?) black shales (anoxia event) ca. 1750 |
C |
Tagragra of Akka |
Anti Atlas Inlier, West African craton |
1755 |
0.03 |
1755 |
0.03 |
1 |
Statherian, (?) black shales (anoxia event) ca. 1750 |
C |
Papilia (Newer Dolerites) |
Singhbhum craton |
1760 |
---- |
1760 |
-9999 |
1 |
Statherian, (?) black shales (anoxia event) ca. 1750 |
C |
Espinhaco |
Amazonian craton |
1770 |
0.05 |
1770 |
0.05 |
1 |
Mid Statherian |
C |
Xionger-Taihang |
North China craton |
1770 |
0.27 |
1770 |
0.27 |
1 |
Mid Statherian |
C |
Libiri |
West African craton |
1790 |
---- |
1790 |
-9999 |
1 |
End Orosirian 1800, FA of sulphidic marine deposits 1780 |
C |
Pebbair |
Dharwar craton |
1788 |
---- |
1788 |
-9999 |
1 |
End Orosirian 1800, FA of sulphidic marine deposits 1780 |
C |
Avanavero |
Amazonia |
1790 |
1.2 |
1790 |
1.2 |
1 |
End Orosirian 1800, FA of sulphidic marine deposits 1780 |
C |
Florida (Uruguayan) |
Rio de la Plata craton |
1790 |
0.03 |
1790 |
0.03 |
1 |
End Orosirian 1800, FA of sulphidic marine deposits 1780 |
C |
Ukrainian AMCG- Prutivka - Novogol |
Sarmatia |
1790 |
0.36 |
1790 |
0.36 |
1 |
End Orosirian 1800, FA of sulphidic marine deposits 1780 |
C |
Hart |
Western Australian craton |
1790 |
2.8 |
1790 |
2.8 |
1 |
End Orosirian 1800, FA of sulphidic marine deposits 1780 |
C |
Hart (Carson-Mount Hay) |
Kimberley block, North Australian craton |
1810-1790 |
0.68 |
1810 |
0.68 |
1 |
End Orosirian 1800, FA of sulphidic marine deposits 1780 |
C |
Eastern Creek |
eastern North Australian craton |
1790-1780 |
---- |
1790 |
-9999 |
1 |
End Orosirian 1800, FA of sulphidic marine deposits 1780 |
C |
Sparrow-Uranium City-Christopher Island |
nw Laurentia |
1833-1818 |
0.35 |
1833 |
0.35 |
1 |
Late Orosirian |
C |
Kalaro-Nimnyrsky-Malozadoiskii |
s Siberian craton |
1870 |
0.58 |
1870 |
0.58 |
1 |
Mid Orosirian, 1880–1870 Ma black shale (anoxia event) |
C |
Black Hills-Soutpansberg |
Kalahari craton |
1880-1840 |
0.04 |
1880 |
0.04 |
1 |
Mid Orosirian, 1880–1870 Ma black shale (anoxia event) |
C |
Circum-Superior (Chukotat, Labrador, Molson-Thompson, Pickle Crow portions) |
Superior craton |
1885-1870 |
0.2 |
1880 |
0.2 |
1 |
Mid Orosirian, 1880–1870 Ma black shale (anoxia event) |
C |
Ghost - Mara River- Morel |
Slave craton |
1890-1870 |
0.21 |
1880 |
0.21 |
1 |
Mid Orosirian, 1880–1870 Ma black shale (anoxia event) |
C |
Mashonaland |
Kalahari craton |
1880 |
0.18 |
1880 |
0.18 |
1 |
Mid Orosirian, 1880–1870 Ma black shale (anoxia event) |
C |
Ramah Group |
Nain portion, North Atlantic craton |
1880 |
---- |
1880 |
-9999 |
1 |
Mid Orosirian, 1880–1870 Ma black shale (anoxia event) |
C |
Bastanar-Hampi |
Indian craton |
1890 |
0.18 |
1890 |
0.18 |
1 |
Mid Orosirian, 1880–1870 Ma black shale (anoxia event) |
C |
Boonadgin |
Yilgarn craton |
1890 |
---- |
1890 |
-9999 |
1 |
Mid Orosirian, 1880–1870 Ma black shale (anoxia event) |
S |
Uatuma |
Amazonia |
1880 |
1.5 |
1880 |
1.5 |
3 |
Mid Orosirian, 1880–1870 Ma black shale (anoxia event) |
C |
Maria-Carajas-Tucumã |
Amazonia |
1880 |
---- |
1880 |
-9999 |
1 |
Mid Orosirian, 1880–1870 Ma black shale (anoxia event) |
Oa |
Flin Flon |
Churchill Province |
ca. 1900 |
---- |
1900 |
-9999 |
2 |
Mid Orosirian |
C |
Hearne |
Slave craton |
1900 |
0.04 |
1900 |
0.04 |
1 |
Mid Orosirian |
C |
Frobisher |
Meta-Incognito block |
ca. 1920 |
0.07 |
1920 |
0.07 |
1 |
Mid Orosirian |
C |
Hartley (Tsineng, Moshaneng) |
Kalahari craton |
1930-1910 |
---- |
1920 |
-9999 |
1 |
Mid Orosirian |
C |
Angaul |
Siberian craton |
1915 |
---- |
1915 |
-9999 |
1 |
Mid Orosirian |
C |
Mugford |
Nain portion, North Atlantic craton |
1950 |
---- |
1950 |
-9999 |
1 |
Mid Orosirian |
C |
Xuwujia |
North China craton |
1960-1930 |
0.03 |
1960 |
0.03 |
1 |
Mid Orosirian |
C |
Khajuraho (Jhansi) |
Bundelkhand craton |
1970 |
0.02 |
1970 |
0.02 |
1 |
Mid Orosirian |
C |
Pechenga-Onega |
Karelian craton |
1970 |
0.5 |
1970 |
0.5 |
1 |
Mid Orosirian |
C |
Xiwangshan |
North China craton |
1970 |
0.01 |
1970 |
0.01 |
1 |
Mid Orosirian |
S |
Orocaima |
Amazonia |
1980-1960 |
0.2 |
1970 |
0.2 |
3 |
Mid Orosirian |
C |
Moi Moi–Charlie-Lucie |
Amazonia |
1985-1975 |
---- |
1980 |
-9999 |
1 |
Mid Orosirian |
C,O |
Minto-Povungnituk |
Superior craton |
1998 |
0.44 |
1998 |
0.44 |
1 |
Early Orosirian |
C |
Kennedy |
Wyoming craton |
2010 |
0.01 |
2010 |
0.01 |
1 |
Early Orosirian |
C |
Lac de Gras-Booth River Igneous Complex (BRIC) |
Slave craton |
2027-2023 |
0.07 |
2030 |
0.07 |
1 |
Early Orosirian |
C |
Cheela Springs |
West Australian craton] |
2031 |
--- |
2031 |
-9999 |
1 |
Early Orosirian |
C |
Union Island-McKee |
Slave craton |
2045-2035 |
--- |
2045 |
-9999 |
1 |
Early Orosirian |
C |
Kangamuit-MD3 |
North Atlantic craton |
2050-2030 |
0.09 |
2050 |
0.09 |
1 |
Early Orosirian |
C |
Bushveld |
Kaapvaal craton |
2060 |
0.39 |
2060 |
0.39 |
1 |
End Rhyacian 2060 (minimum age for the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Keivitsa–Kuetsjärvi-Umba |
Karelia-Kola craton |
2060 |
---- |
2060 |
-9999 |
1 |
End Rhyacian 2060 (minimum age for the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Yixingzhai |
North China craton |
2060 |
0.01 |
2060 |
0.01 |
1 |
End Rhyacian 2060 (minimum age for the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Lac Esprit |
Superior craton |
2070 |
0.07 |
2070 |
0.07 |
1 |
Late Rhyacian (could correspond to the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Voronezh |
Sarmatia |
2070 |
0.2 |
2070 |
0.2 |
1 |
Late Rhyacian (could correspond to the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Fort Frances |
Superior craton |
2075 |
0.17 |
2075 |
0.17 |
1 |
Late Rhyacian (could correspond to the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Palomaa |
Karelian craton |
2070 |
---- |
2070 |
-9999 |
1 |
Late Rhyacian (could correspond to the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Devarabanda |
Dharwar craton |
2080 |
0.07 |
2080 |
0.07 |
1 |
Late Rhyacian (could correspond to the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Cauchon |
Superior craton |
2090 & 2070 |
0.02 |
2090 |
0.02 |
1 |
Late Rhyacian (could correspond to the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Zanhuang-Menglianggu |
North China crato] |
2090 |
---- |
2090 |
-9999 |
1 |
Late Rhyacian (could correspond to the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Snowy Pass |
Wyoming craton |
2100-2080 |
0.01 |
2100 |
0.01 |
1 |
Late Rhyacian (could correspond to the termination of the Lomagundi-Jatuli isotope excursion) |
Oa |
Narracoota |
West Australian craton |
ca. 2100 |
---- |
2100 |
-9999 |
2 |
Late Rhyacian (could correspond to the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Griffin-Kazan-Chipman |
Hearne & Rae cratons |
2116-2111 |
0.14 |
2116 |
0.14 |
1 |
Late Rhyacian (maximum age for the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Bear Mountain |
Wyoming craton |
2115 |
0.02 |
2115 |
0.02 |
1 |
Late Rhyacian (maximum age for the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Tommajarvi-Pirtguba |
Karelian craton |
2115 |
0.11 |
2115 |
0.11 |
1 |
Late Rhyacian (maximum age for the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Haicheng-Xiliu |
[North China craton |
2115-2100 |
---- |
2115 |
-9999 |
1 |
Late Rhyacian (maximum age for the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Marathon |
Superior craton |
2120-2100 |
0.16 |
2120 |
0.16 |
1 |
Late Rhyacian (maximum age for the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Indin |
Slave craton |
2126-2108 |
0.04 |
2126 |
0.04 |
1 |
Late Rhyacian (maximum age for the termination of the Lomagundi-Jatuli isotope excursion) |
C |
Tikkigatsiagak-Avakutak |
North Atlantic craton |
2140-2110 |
0.01 |
2140 |
0.01 |
1 |
Late Rhyacian (peak of the Lomagundi-Jatuli isotope excursion |
C |
Hengling |
North China craton |
2150 |
---- |
2150 |
-9999 |
1 |
Mid Rhyacian (peak of the Lomagundi-Jatuli isotope excursion) |
C |
Rantavaara |
Karelia-Kola craton |
2150 |
0.04 |
2150 |
0.04 |
1 |
Mid Rhyacian (peak of the Lomagundi-Jatuli isotope excursion) |
C |
Riviere du Gue |
Superior craton |
2150 |
0.07 |
2150 |
0.07 |
1 |
Mid Rhyacian (peak of the Lomagundi-Jatuli isotope excursion) |
C |
Biscotasing-Payne River |
Superior craton |
2172-2167 |
0.45 |
2172 |
0.45 |
1 |
Mid Rhyacian (peak of the Lomagundi-Jatuli isotope excursion) |
C |
Wind River & Rabbit Creek – Powder River |
Wyoming craton |
2170 & 2155 |
---- |
2170 |
-9999 |
1 |
Mid Rhyacian (peak of the Lomagundi-Jatuli isotope excursion) |
C |
Mahbubngour - Dandeli |
Dharwar craton |
2180 |
0.29 |
2180 |
0.29 |
1 |
Mid Rhyacian (peak of the Lomagundi-Jatuli isotope excursion) |
C |
SW Slave Province (Dogrib) |
Slave craton |
2193-2180 |
0.04 |
2193 |
0.04 |
1 |
Mid Rhyacian (peak of the Lomagundi-Jatuli isotope excursion) |
C |
Tulemalu-MacQuoid |
Rae craton |
2190 |
0.04 |
2190 |
0.04 |
1 |
Mid Rhyacian (peak of the Lomagundi-Jatuli isotope excursion) |
Oa |
Man-Leo |
West African craton |
2250-2000 |
---- |
2250 |
-9999 |
2 |
|
C |
Malley & MacKay |
Slave craton |
2230 & 2210 |
0.07 |
2210 |
0.07 |
1 |
Early Rhyacian, Rietfontein glaciation ca. 2220; minimum age for the start of the Lomagundi- Jatuli carbon isotope excursion |
C |
Koli (Karjalitic sills) |
Karelia-Kola craton |
2215 |
0.1 |
2215 |
0.1 |
1 |
Early Rhyacian, Rietfontein glaciation ca. 2220; minimum age for the start of the Lomagundi- Jatuli carbon isotope excursion |
C |
Anantapur-Kunigal |
Dharwar craton |
2215 |
0.24 |
2215 |
0.24 |
1 |
Early Rhyacian, Rietfontein glaciation ca. 2220; minimum age for the start of the Lomagundi- Jatuli carbon isotope excursion |
C |
Kandlamadugu |
Dharwar craton |
2220 |
0.41 |
2220 |
0.41 |
1 |
Early Rhyacian, Rietfontein glaciation ca. 2220; minimum age for the start of the Lomagundi- Jatuli carbon isotope excursion |
C |
Ungava-Nipissing |
Superior craton |
2220-2210 |
0.58 |
2220 |
0.58 |
1 |
Early Rhyacian, Rietfontein glaciation ca. 2220; minimum age for the start of the Lomagundi- Jatuli carbon isotope excursion |
C |
BN-1 |
North Atlantic craton |
2225 |
0.04 |
2225 |
0.04 |
1 |
Early Rhyacian, Rietfontein glaciation ca. 2220; minimum age for the start of the Lomagundi- Jatuli carbon isotope excursion |
C |
Turee Creek |
Pilbara craton |
2215 |
---- |
2215 |
-9999 |
1 |
Early Rhyacian, Rietfontein glaciation ca. 2220; minimum age for the start of the Lomagundi- Jatuli carbon isotope excursion |
C |
Vestfold Hills-2 |
Antarctica |
2240 |
0.01 |
2240 |
0.01 |
1 |
Early Rhyacian |
C |
Ippaguda |
Dharwar craton |
2250 |
0.08 |
2250 |
0.08 |
1 |
Early Rhyacian |
C |
Kaptipada |
Singhbhum craton |
2250 |
0.02 |
2250 |
0.02 |
1 |
Early Rhyacian |
C |
Hekpoort |
Kaapvaal craton |
ca. 2250 |
0.2 |
2250 |
0.2 |
1 |
Early Rhyacian |
C |
Tailvalkovski-Kuito |
Karelia-Kola craton |
2330-2310 |
0.02 |
2330 |
0.02 |
1 |
End Siderian 2300, Gowganda-Rooihoogte glaciation ca. 2330 |
C |
Bangalore-Karimnagar |
Dharwar & Bastar cratons |
2365 |
0.26 |
2365 |
0.26 |
1 |
Mid Siderian, Bruce-Duitschland glaciation ca. 2370 |
C |
Graedefjord- Scourie |
North Atlantic craton |
2420-2365 |
---- |
2420 |
-9999 |
1 |
Mid Siderian, Bruce-Duitschland glaciation ca. 2370 |
C |
Dantewara |
Bastar craton |
ca. 2400 |
0.06 |
2400 |
0.06 |
1 |
Mid Siderian |
C |
Widgiemooltha (-Erayinia) |
Yilgarn craton |
2420-2410 |
0.45 |
2420 |
0.45 |
1 |
Mid Siderian |
C |
Sebanga Poort |
Zimbabwe, Kaapvaal craton |
2420 |
---- |
2420 |
-9999 |
1 |
Mid Siderian |
C |
Ringvassoy |
Norrbotten block |
2410 |
---- |
2410 |
-9999 |
1 |
Mid Siderian |
C |
Uoleviniehto – Imandra |
Karelian craton |
2400 |
---- |
2400 |
-9999 |
1 |
Mid Siderian |
C |
du Chef |
Superior craton |
2400 |
---- |
2400 |
-9999 |
1 |
Mid Siderian |
C |
Ongeluk |
Kaapvaal craton |
2425 |
0.2 |
2425 |
0.2 |
1 |
Mid Siderian, initiation of Ramsey Lake-Makganyene glaciation ca. 2430 |
C |
Welli Wolli - Woongara |
Pilbara craton |
2450 |
0.04 |
2450 |
0.04 |
1 |
Early Siderian |
C |
Matachewan |
Superior craton |
2460 (+2480) |
0.56 |
2460 |
0.56 |
1 |
Early Siderian |
C |
BLIP-2 (Baltic LIP-young) (Pääjärvi) |
Karelia-Kola craton |
2445 |
0.28 |
2445 |
0.28 |
1 |
Early Siderian |
C |
Blue Draw |
Wyoming craton |
2480 |
0.01 |
2480 |
0.01 |
1 |
Early Siderian |
C |
Kaminak |
Hearne craton |
2498 |
0.03 |
2498 |
0.03 |
1 |
End Archean 2500 |
C |
BLIP -1 (Baltic LIP-old) |
Karelia-Kola craton |
2505 |
0.28 |
2505 |
0.28 |
1 |
End Archean 2500 |
C |
Crystal Springs |
Zimbabwe craton |
2510 |
---- |
2510 |
-9999 |
1 |
End Archean 2500 |
C |
Mistassini-Ptarmigan-Irsuaq |
Superior craton |
2510-2500 |
0.11 |
2510 |
0.11 |
1 |
End Archean 2500 |
C |
Great Dyke of Zimbabwe |
Zimbabwe craton |
2575 |
0.07 |
2575 |
0.07 |
1 |
Late Neoarchean |
C |
Stockford |
Limpopo belt |
2605 |
2605 |
-9999 |
1 |
Late Neoarchean |
|
C |
Yandinilling |
Yilgarn craton |
2620 |
2620 |
-9999 |
1 |
Late Neoarchean |
|
C |
Aousserd-Tichla |
Reguibat craton |
2670 |
---- |
2670 |
-9999 |
1 |
Mid Neoarchean, iron formations |
C |
Stillwater- Rendevous |
Wyoming craton |
2710-2680 |
0.07 |
2710 |
0.07 |
1 |
Mid Neoarchean, iron formations |
C,O? |
Abitibi belt |
Superior craton |
2750-2680 |
---- |
2750 |
-9999 |
1 |
Mid Neoarchean, iron formations |
C,O |
Allanridge (younger Ventersdorp) |
Kaapvaal craton |
2720-2680 |
---- |
2720 |
-9999 |
1 |
Mid Neoarchean, iron formations |
C |
Maddina (part of Fortescue) |
Pilbara craton |
2715 |
0.14 |
2715 |
0.14 |
1 |
Mid Neoarchean, iron formations |
C,O |
Eastern Goldfields & Gnanagooragoo-Yalgowra |
Yilgarn craton |
2750-2710 |
---- |
2750 |
-9999 |
1 |
Mid Neoarchean, iron formations |
C |
Kam Group |
Slave craton |
2730-2680 |
---- |
2730 |
-9999 |
1 |
Mid Neoarchean, iron formations |
C |
Prince Albert |
Rae craton |
2700 |
---- |
2700 |
-9999 |
1 |
Mid Neoarchean, iron formations |
C,O? |
Bulawayan-Zeederberg-Belingwe |
Zimbabwe craton |
ca. 2710 |
---- |
2710 |
-9999 |
1 |
Mid Neoarchean, iron formations |
C |
Uaua |
Sao Francisco craton |
2730 & 2625 |
---- |
2730 |
-9999 |
1 |
Mid Neoarchean, iron formations |
C |
Ahmeyim (includes Great Dyke of Mauritania) |
Reguibat craton |
2733 |
0.1 |
2733 |
0.1 |
1 |
Mid Neoarchean |
C |
Kathleen Valley (-Kylena) (middle Fortescue) |
Pilbara craton |
2740 |
0.14 |
2740 |
0.14 |
1 |
Mid Neoarchean |
C |
Ring of Fire & Bird River |
Superior craton |
2740-2730 |
0.04 |
2740 |
0.04 |
1 |
Mid Neoarchean |
C |
Serra Leste Magmatic Suite |
Carajas block |
2750 |
---- |
2750 |
-9999 |
1 |
Mid Neoarchean |
C |
Sylvania Inlier |
Pilbara craton |
2750 |
---- |
2750 |
-9999 |
1 |
Mid Neoarchean |
C |
Black Range - Mount Roe (older Fortescue) |
Pilbara craton |
2780 |
0.13 |
2780 |
0.13 |
1 |
End Mesoarchean 2800 |
C |
Klipriviersberg -(older Ventersdorp) |
Kaapvaal craton |
2780 |
0.39 |
2780 |
0.39 |
1 |
End Mesoarchean 2800 |
Oa |
Vizien |
ne Superior craton |
2785 |
---- |
2785 |
-9999 |
2 |
End Mesoarchean 2800 |
C |
Meeline-Norie-Windimurra-Little Gap |
Yilgarn craton |
2810-2790 |
---- |
2810 |
-9999 |
1 |
End Mesoarchean 2800 |
C |
Hlagothi |
Kaapvaal craton |
2860 |
0.03 |
2860 |
0.03 |
1 |
Late Mesoarchean |
C |
Radley |
Pilbara craton |
2920 |
---- |
2920 |
-9999 |
1 |
Mid Mesoarchean |
C |
Steep Rock |
North Caribou terrane, Superior craton |
2930 |
---- |
2930 |
-9999 |
1 |
Mid Mesoarchean |
C |
Balmer |
North Caribou terrane, Superior craton |
2990 |
---- |
2990 |
-9999 |
1 |
Mid Mesoarchean |
C |
Nsuze (Ushushwana, Barberton-Badplaas |
Kaapvaal craton |
2990-2980 |
---- |
2990 |
-9999 |
1 |
Mid Mesoarchean |
S |
Gavião |
Gavião Block |
3300 |
---- |
3300 |
-9999 |
3 |
Paleo-Archean |
C |
Onverwacht (Komati, Hooggenoeg, Kromberg fm) |
Kaapvaal craton |
3490-3330 (multiple pulses) |
---- |
3490 |
-9999 |
1 |
Paleo-Archean |
Notes:
Locations: w = west, ne = northeast, etc.
Ages: In most cases, ages are quoted to the nearest 5 myr. Those with uncertainties > 10 myr are preceded by “ca.”
Area: areal estimates were not available in all cases, and in most of those cases, the size is small and we are interpreting these as fragments of LIPs.
LIP type: C= continental; O = oceanic, O = accreted accreted, S = Silicic.
Grey shaded columns (Age, Area, LIP type) contain numeric data for database use
LIP type (numeric): 1 = continental LIP, 2 = oceanic LIP, 3 = Silicic LIP.
Area (numeric): -9999 =no data.