2001
DOI: 10.1007/bf02910304
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Evolution of the Paleo-Asian Ocean (Altai-Sayan Region, Central Asia) and collision of possible Gondwana-derived terranes with the southern marginal part of the Siberian continent

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Cited by 267 publications
(189 citation statements)
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“…Microcontinents and continental fragments are considered to have been incorporated into the CAOB during its accretion (Windley et al, 2007;Gao et al, 2011;Kröner et al, 2012;Alexeiev et al, 2015;Zhang et al, 2015aZhang et al, ,b,c, 2016. However, their origins are still controversial, with some researchers assuming that some microcontinents within the CAOB had a Gondwana derivation and were then accreted onto the southern margin of the Siberian Craton (Zonenshain et al, 1990;Buslov et al, 2001;Dobretsov et al, 2003;Kheraskova et al, 2003;Laurent-Charvet et al, 2003;Xiao et al, 2010). In contrast, models that favor the origin of the Siberian Craton have been proposed recently (Berzin and Dobretsov, 1994;Sengör and Natal'in, 1996;Kuzmichev et al, 2001;Turkina et al, 2007;Zhou et al, 2009Zhou et al, , 2010aZhou et al, ,b,c, 2011.…”
Section: Introductionmentioning
confidence: 99%
“…Microcontinents and continental fragments are considered to have been incorporated into the CAOB during its accretion (Windley et al, 2007;Gao et al, 2011;Kröner et al, 2012;Alexeiev et al, 2015;Zhang et al, 2015aZhang et al, ,b,c, 2016. However, their origins are still controversial, with some researchers assuming that some microcontinents within the CAOB had a Gondwana derivation and were then accreted onto the southern margin of the Siberian Craton (Zonenshain et al, 1990;Buslov et al, 2001;Dobretsov et al, 2003;Kheraskova et al, 2003;Laurent-Charvet et al, 2003;Xiao et al, 2010). In contrast, models that favor the origin of the Siberian Craton have been proposed recently (Berzin and Dobretsov, 1994;Sengör and Natal'in, 1996;Kuzmichev et al, 2001;Turkina et al, 2007;Zhou et al, 2009Zhou et al, , 2010aZhou et al, ,b,c, 2011.…”
Section: Introductionmentioning
confidence: 99%
“…Sengör et al, 1993;Windley et al, 2007;Cawood et al, 2009), during which various terrains (e.g. ophiolites, seamounts, island arcs and microcontinents) were accreted onto the southern margin of the Siberia Craton (Buslov et al, 2001;Badarch et al, 2002;Khain et al, 2003;Kuzmichev et al, 2005;Windley et al, 2007;Kelty et al, 2008;Xiao et al, 2008Xiao et al, , 2009). Long-lasting accretionary process results in mélanges, disorder of regional stratigraphy and development of thrust faults, while subduction of oceanic crust brings crustal materials into mantle and enhances intensive crust-mantle interactions (Sengör and Natal'in, 1996).…”
Section: Introductionmentioning
confidence: 99%
“…The recent results from detailed geological mapping, structural analysis and geochronological studies [Buslov et al, 2001[Buslov et al, , 2003Korobkin, Buslov, 2011;Smirnova et al, 2002;Cai et al, 2011aCai et al, , 2011bCai et al, , 2011cCai et al, , 2014Chen et al, 2015] were used to identify the following tectonic elements of the Central Asian fold belt [Buslov, 2011;Dobretsov, Buslov, 2007, 2011Buslov et al, 2013] (Fig. 1):…”
Section: P a L E O G E O D Y N A M I C Smentioning
confidence: 99%