Age, composition, and tectonic significance of Palaeozoic granites in the Altyn orogenic belt, China. Chunhua Liu MLR Key Laboratory of Metallogeny and Mineral ... PR China;State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, PR China Correspondence …
به خواندن ادامه دهیدThe North China Craton (NCC) is one of the oldest cratonic blocks in the world as old as 4.0 Ga (Wan et al., 2021), which is bounded by the Central Asian Orogenic Belt to the north and the Qinling-Dabie and Sulu Orogenic belts to the south (Fig. 1 a) (Liu et al., 2008, Wu et al., 2008, Zhai and Santosh, 2011, Zhai, 2014).There is a broad consensus that the NCC was …
به خواندن ادامه دهیدA number of Late Mesozoic (∼130 Ma) A-type granitic plutons have been identified in Southeast China.Here we investigate the petrogenesis of one of these granitic plutons in Southeast China, the Sanqingshan–Damaoshan (SD) granites in northeastern Jiangxi Province, using zircon U–Pb geochronology, Hf isotopic analyses, and major and trace element analyses.
به خواندن ادامه دهیدWe have identified a new crustally derived granite pluton that is related to the Emeishan Large Igneous Province (ELIP). This pluton (the Wase pluton, near Dali) shows two distinct SHRIMP zircon U–Pb age groups (~768 and ~253 Ma). As it has an intrusive relationship with Devonian limestone, the younger age is interpreted as its formation, which is related to …
به خواندن ادامه دهیدThe geochemical comparation shows that the South China granites share similar REE contents with those of many granites from places outside South China. Such similarity has also been found between REE ore-related and ore-barren granites in South China. This shows that granites from outside South China could also have ore-forming potential.
به خواندن ادامه دهیدTherefore, the compiled papers basically represent the current level of research on weathered granites in South China. Download: Download full-size image; Fig. 1. Distribution of granites in China. Granites are mainly distributed in areas of South China, especially in the areas of Guangdong, Fujian, Southeast of Guangxi and south of Hunan.
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به خواندن ادامه دهیدHuang, Highly fractionated S-type granites from the giant Dahutang tungsten deposit in Jiangnan Orogen, Southeast China: geochronology, petrogenesis and their relationship with W-mineralization, Lithos, № 202, с. 207 ... Zhai, Metallogeny of the North China Craton: link with secular changes in the evolving Earth, Gondwana Res., № 24, с. 275
به خواندن ادامه دهیدThe 2.31 Ga Low δ 18 O granites were related to partial melting of high-T hydrothermal altered crustal rocks in a rift.. The weaker low-18 O signatures of the 2.18 Ga granites were inherited from the 2.31 Ga granites.The southern TNCO went through tectonic switch from continental rift to active continental margin during 2.3–2.1 Ga.
به خواندن ادامه دهیدHuashan, Guposhan and Qitianling are three similar and representative metaluminous A-type tin granites in the western Nanling Range, China. They all have a high oxidization state with magnetite as the dominant Fe–Ti oxide. This study presents an understanding of systematic mineralogy of Sn-bearing minerals (biotite, titanite, magnetite and ...
به خواندن ادامه دهیدWe present the first evidence of late Pan-African magmatism in the Jiamusi Massif of northeastern China. Recent SHRIMP U–Pb zircon studies of the Mashan Complex have identified a major ∼500 Ma granulite facies metamorphic event in the area, but no older igneous rocks have previously been dated.Two granitoid samples have been analysed using SHRIMP …
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به خواندن ادامه دهیدNortheast China is situated within a significant Phanerozoic accretionary orogenic belt, located in the eastern section of the Central Asian Orogenic Belt (Sengör et al., 1993, Jahn et al., 2000).At present, a polymetallic metallogenic province (including Narenwula, Baiyinhan, Weilasituo, Baiyinchagan, Dongshanwan, Chaihulanzi, Zhaojinggou, Bainaimiao, Sadaigoumen) has been …
به خواندن ادامه دهیدTherefore, the compiled papers basically represent the current level of research on weathered granites in South China. Section snippets Geochemical types. The formation and evolution of weathering profiles in humid tropic areas is essentially a geochemical process (Huang et al., 1996). In terms of geochemical types, weathering profiles in China ...
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به خواندن ادامه دهیدThe South China is tectonically divided into two major blocks: the Yangtze Block to the northwest and the Cathaysia Block to the southeast (Fig. 1).The rocks of the ca. 2.9 Ga Kongling complex (Gao et al., 1999, Qiu et al., 2000, Zheng et al., 2006, Zhang et al., 2006) are considered to be the oldest in the Yangtze Block.Although there are no reports of Archean …
به خواندن ادامه دهیدNE China is composed of a Paleozoic orogenic collage that is considered to be the eastern part of the CAOB (Sengör et al., 1993, Sengör and Natal'in, 1996, Jahn et al., 2000a).It has previously been suggested that this orogenic segment has undergone two stages of evolution under different tectonic regimes (Wu et al., 2002).In the Paleozoic, tectonic development was …
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به خواندن ادامه دهیدThe Qinling Orogen in central China is a complex collage built through the closure of the northernmost Paleo-Tethys and the suturing of the Yangtze and the North China cratons. ... extensive Late Mesozoic granitoids were emplaced, with an age range of 108–160 Ma. They are dominated by I-type granites that indicate formation through remelting ...
به خواندن ادامه دهیدLow-δ18O A-type granites in SW China Geological Society of America Bulletin, v. 130, no. XX/XX 3 thickness ranging from several hundred meters in the east (e.g., Guizhou) to 5000m in the west
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به خواندن ادامه دهیدA typical example is the North China Craton (NCC) which hosts a large volume of Late Mesozoic granites that formed far distance (>1000 km) from the Paleo-Pacific plate margin (Fig. 1) 4 – 6. More interestingly, these intracontinental granites, particularly the Early Cretaceous ones, contain abnormally higher water contents in zircon than ...
به خواندن ادامه دهیدSIMS zircon U Pb ages are 157 ± 1 Ma, 161 ± 3 Ma, 159 ± 2 Ma and 158 ± 2 Ma respectively. The Xihuashan granites are high evolved I–S transformation-type. Granites were derived from Late Paleo proterozoic to Early Mesoproterozoic lower crust. Fluid/melt interaction produces REE tetrad effect in the second and third phases. Late Jurassic W Sn deposits in SE …
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به خواندن ادامه دهیدThe Jurassic granites in South China, which mainly consist of biotite granite, two-mica granite and muscovite granite, have already been differentiated into S- and I-type by previous studies (Chen and Jahn, 1998; Zeng et al., 2001; Hua et al., 2003; Yang et al., 2016). The S-type granites were interpreted to be derived from the regional ...
به خواندن ادامه دهیدRecycled lower oceanic crust signal in early Jurassic A 1-type granites, South China: Implications for flat-slab subduction and mantle heterogeneity in the continental back-arc region. Author links open overlay panel Bo Yan a b, Wu-Xian Li a, Xiao-Long Huang a, Ji-Hua Tao c d. Show more.
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