2016
DOI: 10.1016/j.chemgeo.2016.05.011
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Early Cretaceous potassic volcanic rocks in the Jiangnan Orogenic Belt, East China: Crustal melting in response to subduction of the Pacific–Izanagi ridge?

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Cited by 35 publications
(19 citation statements)
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References 84 publications
(149 reference statements)
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“…Extensive extrusive and intrusive magmatic activity occurred in the GHB during the Early Cretaceous for available Ar‐Ar, K‐Ar, and zircon U‐Pb data defining an age peak at ca. 130 Ma (Hu et al, ; Jiang et al, , ; Peng et al, ; Qi et al, , ; Shu et al, ; Sun et al, ; Wong et al, ; Xia et al, ; Xiang et al, ; Yang et al, ; L. Zhao et al, ; Zhou et al, ). The mafic magmatic rocks in the GHB are characterized by variable isotopic compositions [( 87 Sr/ 86 Sr) i = 0.70354–0.71086; ε Nd ( t ) = −10.4 to +6.6; Table S6 in the supporting information; Jiang et al, ; Qi et al, , ; Shu et al, ; Xia et al, ].…”
Section: Geological Setting and Petrographymentioning
confidence: 99%
“…Extensive extrusive and intrusive magmatic activity occurred in the GHB during the Early Cretaceous for available Ar‐Ar, K‐Ar, and zircon U‐Pb data defining an age peak at ca. 130 Ma (Hu et al, ; Jiang et al, , ; Peng et al, ; Qi et al, , ; Shu et al, ; Sun et al, ; Wong et al, ; Xia et al, ; Xiang et al, ; Yang et al, ; L. Zhao et al, ; Zhou et al, ). The mafic magmatic rocks in the GHB are characterized by variable isotopic compositions [( 87 Sr/ 86 Sr) i = 0.70354–0.71086; ε Nd ( t ) = −10.4 to +6.6; Table S6 in the supporting information; Jiang et al, ; Qi et al, , ; Shu et al, ; Xia et al, ].…”
Section: Geological Setting and Petrographymentioning
confidence: 99%
“…The Qinling‐Dabie‐Sulu Orogen is located to the north margin of the SCB, which is adjoined to the Indosinian Block by the Red River Fault to the southwest (Li, Santosh, Zhao, Zhang, & Jin, ; K. Qiu & Deng, ; K. Qiu, Marsh, Yu, Pfaff, Gulbransen, Gou, & Li, ; K. Qiu et al, ). The Yangtze and Cathaysia blocks were amalgamated together to form the united SCC during the late Neoproterozoic (D. Xu et al, ; Yao, Shu, & Santosh, ; Yao, Shu, Santosh, & Li, ; Yao, Shu, Cawood, & Li, ; Yin et al, ; L. Zhao, Guo, et al, ; K. Zhao, Jiang, et al, ). However, during the later Neoproterozoic and early‐middle Ordovician, the SCB split again, resulting in a complex intracontinental rift arrangement (K. Qiu et al, ).…”
Section: Regional Geologymentioning
confidence: 99%
“…Abundant syntectonic granite intrusions are distributed in the deeper basement at the center of the Yunkai Massif, including charnockite intrusions with zircon U–Pb ages ranging from 448 to 405 Ma (C. Chen et al, ; Lin, Wang, & Chen, ; D. Wang et al, ; Figure ). The Indosinian magma mainly produced a series of Al‐rich granites (including cordierite and garnet), which are generally NE–SW‐trending along the western side of the Luchuan‐Cenxi Fault and the eastern side of the Wuchuan‐Sihui Fault; their zircon U–Pb ages mainly range from 242 to 220 Ma (C. Chen et al, ; L. Zhao, Guo, et al, ; K. Zhao, Jiang, et al, ; Zhong et al, ; Figure ). The Yanshanian intrusions are mainly distributed along the Wuchuan‐Sihui Fault (Lin et al, ).…”
Section: Regional Geologymentioning
confidence: 99%
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