2017
DOI: 10.1007/s12583-017-0730-z
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Zircon U-Pb age, geochemical data: Constraints on the origin and tectonic evolution of the metamafic rocks from Longmuco-Shuanghu-Lancang suture zone, Tibet

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Cited by 16 publications
(7 citation statements)
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“…The existence of zircon in rocks is useful for dating them [247] and the presence of zircon in the continental crust and oceanic ridges make it a very important material to test geological models [248]. In addition, the properties of this mineral are used to impose constraints on the origin and tectonic evolution of the metamorphic rocks [249] and to study the formation of granites by melting of the igneous crust [250]. For all these purposes, it is quite important to understand the stability of zircon at very high pressures.…”
Section: Technological and Geophysical Implicationsmentioning
confidence: 99%
“…The existence of zircon in rocks is useful for dating them [247] and the presence of zircon in the continental crust and oceanic ridges make it a very important material to test geological models [248]. In addition, the properties of this mineral are used to impose constraints on the origin and tectonic evolution of the metamorphic rocks [249] and to study the formation of granites by melting of the igneous crust [250]. For all these purposes, it is quite important to understand the stability of zircon at very high pressures.…”
Section: Technological and Geophysical Implicationsmentioning
confidence: 99%
“…This belt records the process of subduction–collision and exhumation of the Yangtze Plate and Gondwana (Zhai et al . 2009, 2011 a ; Wu, 2013) (Fig. 1b).…”
Section: Geological Backgroundmentioning
confidence: 98%
“…2010; Hu et al . 2013; Wu, 2013). In the NQB, the Riwanchaka Formation (a series of marine Carboniferous rocks) is exposed in the Chabu area and is rich in fossil corals, brachiopods and ammonites (Xie, 1983).…”
Section: Introductionmentioning
confidence: 99%
“…This belt contains low‐metamorphic grade pre‐Permian basement rocks (Kapp et al, 2003; Liu et al, 2017; Zhang et al, 2013; Zhao et al, 2015), as well as a Triassic mélange with inclusions and rafts that range in size from cm to km. Inclusion lithologies are highly variable, including mafic rocks (ages range from 272 to 505 Ma; Wu et al, 2017; Zhai et al, 2013, 2016;), low‐grade metasediments, including Permian limestones, as well as HP‐rocks, mainly blueschists and eclogites (Kapp et al, 2000; Li, Zhai, Dong, & Huang, 2006; Pullen et al, 2010; Pullen & Kapp, 2014; Zhai et al, 2011; Zhang et al, 2006, 2010). The matrix of the mélange, however, appears of low‐metamorphic grade at the most (Zhao et al, 2014, 2015).…”
Section: Geologic Backgroundmentioning
confidence: 99%