首页|Corrigendum to “Petrogenesis and geochronology of Paleoproterozoic magmatic rocks in the Kongling complex: Evidence for a collisional orogenic event in the Yangtze craton” [Lithos 342–343 (2019) 513–529] (LITHOS (2019) 342–343 (513–529), (S0024493719301999), (10.1016/j.lithos.2019.05.015))
Corrigendum to “Petrogenesis and geochronology of Paleoproterozoic magmatic rocks in the Kongling complex: Evidence for a collisional orogenic event in the Yangtze craton” [Lithos 342–343 (2019) 513–529] (LITHOS (2019) 342–343 (513–529), (S0024493719301999), (10.1016/j.lithos.2019.05.015))
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NSTL
Elsevier
? 2021 Elsevier B.V.The authors regret that the tectonic setting discrimination diagrams (Fig. 12a) in this article have an obvious mistake that the horizontal and vertical axes (Nb and Y contents in ppm) should be exchanged. The corrected Fig. 12 is attached below. [Figure presented] Fig. 12. (a) and (b) Tectonic setting discrimination diagrams of Nb vs. Y and Y + Nb vs. Rb; (c) and (d) subtype classification of A-type granites. Abbreviations: VAG = volcanic arc granites; ORG = ocean ridge granites; WPG = within-plate granites; Syn-COLG and Post-COLG = syn- and post-collisional granites; OIB = oceanic island basalt; IAB = island arc basalt; A1 = granitoids in anorogenic settings; A2 = post-orogenic granites emplaced after a continental collision. Panels (a) and (b) are after Pearce et al. (1984, 1996). A-type granites field in panel (c) is after Whalen et al. (1987), panels (c) and (d) after Eby (1992). Data sources are the same as in Fig. 7. The authors would like to apologise for any inconvenience caused.
Han Q.、Peng S.、Polat A.、Kusky T.
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Hubei Key Laboratory of Critical Zone Evolution Center for Global Tectonics School of Earth Sciences State Key Laboratory of Geological Processes and Mineral Resources China University of Geosciences
NSTL
Elsevier
