Titlebook: Mafic-ultramafic Intrusions in Beishan and Eastern Tianshan at Southern CAOB: Petrogenesis, Minerali; Ben-Xun Su Book 2014 Springer-Verlag

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Introduction,east and from the Siberian Craton in the north to the Tarim Craton in the south (Fig. 1.1; Sengör et al. in Nature 364:299–307, 1993; Jahn et al. in Research of Society Edinburgh: Earth Science 91:181–193, 2000a; Episodes 23:82–92, 2000b; Journal of Asian Earth Sciences 23:599–603, 2004; Windley et

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Geochemistry, (Na.O + K.O) are positively correlated with SiO. (Fig. 6.1). The dunites have the lowest SiO. (36.3–40.1 wt%), CaO (0.23–5.06 wt%), and Na.O (0.03–0.46 wt%) and the highest MgO (26.4–38.6 wt%), TFeO (total Fe; 6.61–12.1 wt%), and MnO (0.13–0.19 wt%) contents. Among the dunites, the plagioclase-bear

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Concluding Remarks,of mafic–ultramafic intrusions and series of discoveries of magmatic Ni–Cu deposits are attracting the attention from geologists. This thesis focused on five intrusions of the Beishan region, namely: Hongshishan, Xuanwoling, Bijiashan, Poshi and Luodong. It involved the petrologic, mineralogical, ge

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Introduction,s 328:15–51, 2000; Jahn et al. in Episodes 23:82–92, 2000b; Journal of Asian Earth Sciences 23:599–603, 2004; Xiao et al. in Tectonics 22:1069, 2003; Sun et al. in Chemical Geology 247:352–383, 2008; Wong et al. in Gondwana Research 18:438–454, 2010). The tectonic evolution of Chinese Tianshan, part

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ance to the perioperative management with extensive background and clinical evidence to allow the reader gain an in –depth understanding of this complex and fascinating topic..978-1-4939-4101-8978-1-4614-5167-9