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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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發(fā)表于 2025-3-23 11:28:49 | 只看該作者
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發(fā)表于 2025-3-23 13:56:20 | 只看該作者
Introduction,east and from the Siberian Craton in the north to the Tarim Craton in the south (Fig.?1.1; Seng?r 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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發(fā)表于 2025-3-23 18:45:43 | 只看該作者
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發(fā)表于 2025-3-24 04:43:22 | 只看該作者
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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發(fā)表于 2025-3-24 06:43:03 | 只看該作者
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發(fā)表于 2025-3-24 11:03:31 | 只看該作者
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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發(fā)表于 2025-3-24 16:15:36 | 只看該作者
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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發(fā)表于 2025-3-24 19:23:05 | 只看該作者
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發(fā)表于 2025-3-25 03:13:40 | 只看該作者
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
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