2014
DOI: 10.1016/j.lithos.2014.08.024
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Timing, petrogenesis and tectonic setting of the Late Paleozoic gabbro–granodiorite–granite intrusions in the Shalazhashan of northern Alxa: Constraints on the southernmost boundary of the Central Asian Orogenic Belt

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Cited by 90 publications
(73 citation statements)
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“…[Zhang et al, 2013;Shi et al, 2014aShi et al, , 2014b), and granitoids in the south belt formed from the late stage of Early Paleozoic to the Late Permian (e.g. [Li, 2006;Dan et al, 2016]).…”
Section: P a L E O G E O D Y N A M I C Smentioning
confidence: 99%
See 1 more Smart Citation
“…[Zhang et al, 2013;Shi et al, 2014aShi et al, , 2014b), and granitoids in the south belt formed from the late stage of Early Paleozoic to the Late Permian (e.g. [Li, 2006;Dan et al, 2016]).…”
Section: P a L E O G E O D Y N A M I C Smentioning
confidence: 99%
“…This indicates that the granitoids in the two belts have different sources: the source for the north belt granitoids is generally juvenile and the source for the south belt granitoids consists of more old materials. Therefore, the north belt could not be a part of the Alxa block [Shi et al, 2014a[Shi et al, , 2014bZhang et al, 2015].…”
mentioning
confidence: 99%
“…This indicates that the ZS zone is most likely a constituent part of the southern CAOB. This inference is further reinforced by whole-rock Nd isotopic studies of Phanerozoic granitoids and volcanic rocks (Yarmolyuk et al, 2007;Dolgopolova et al, 2013;Shi et al, 2014a) and similar Hf-in-zircon isotopes for the ZS zone and the southern CAOB (Fig. 9b).…”
Section: Constraints On the Southern Boundary Of The Caobmentioning
confidence: 63%
“…The zircon xenocrysts from the WNCC are from (Pi et al, 2010;Wu et al, 2013). Previous Hf isotopic data of intrusive rocks in ZS zone cited after Shi et al (2014aShi et al ( , 2014b. Hf isotopic data of Precambrian rocks in ZS zone cited after Shi (2015).…”
Section: Tracking Of Deep Crustal Composition Using Zircon Xenocrystsmentioning
confidence: 98%
“…The annual amount of evaporation is as high as 30-times the rainfall in this area; hence, it is an extremely arid region with very few people living there [13]. According to the tectonic analyses, this area is situated in the region between the central part of the southern Central Asian Orogenic Belt (CAOB) and the Alxa Block [14,15]. Velocity field of crustal movement based on GPS shows that the crust is relatively stable in Alxa area ( Figure 2) [16].…”
Section: Introductionmentioning
confidence: 98%