Petrogenesis and tectonic significance of the Early Devonian lamprophyres and diorites in the Alxa Block,NW China |
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| Institution: | 1. State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang, 330013, Jiangxi, China;2. Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha, 410083, China;3. School of Geosciences and Info-Physics, Central South University, Changsha, 410083, China;4. College of Goegraphic Science, Xinyang Normal University, Xinyang, Henan, 464000, China;5. Nickel Cobalt Research and Design Institute, Jinchuan Group Co., Ltd., Jinchang, Gansu, 737104, China |
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| Abstract: | The North Qilian orogenic belt (NQOB) has been defined as a subduction-collision zone between the Alxa Block and the Qilian Block during the Early Paleozoic. To constrain the post-collisional tectonic evolution of the NQOB, analyses of zircon U-Pb-Hf isotopes, whole-rock major, trace element and Sr-Nd-Pb isotope compositions of the newly discovered Early Devonian lamprophyres and diorites dikes from the Longshoushan area in southwestern margin of the Alxa Block were conducted. Zircon U-Pb dating yields emplacement ages of 400 ± 4 Ma and 403 ± 6 Ma for two lamprophyre dikes and 391 ± 3 Ma for two diorite dikes. The lamprophyres dikes are shoshonitic-high-K (calc-alkaline) in nature, and are characterized by SiO2 contents of 53.6–56.3 wt %, (87Sr/86Sr)i ratios of 0.7064 to 0.7072, εNd(t) values of 0.1–1.0, and zircon εHf(t) values of ?8.0 to ?2.9. The diorite dikes are high-K (calc-alkaline), and are characterized by MgO contents of 6.32–6.98 wt %, (87Sr/86Sr)i ratios of 0.7089–0.7137, εNd(t) values of ?3.8 to ?3.5, and zircon εHf(t) values of ?9.9–0.4. Both the lamprophyre and diorite dikes show parallel enrichments in LREEs and LILEs and depletions in HREEs and HFSEs and have similar ratios of (206Pb/204Pb)i (17.587–18.133), (207Pb/204Pb)i (15.518–15.584) and (208Pb/204Pb)i (37.676–38.058). Geochemical and isotopic data suggest that the lamprophyre and diorite dikes were derived from low-degrees melts of amphibole- and phlogopite-bearing lherzolite and phlogopite-bearing lherzolite, respectively, in the spinel-garnet transition facies. Their parental magmas both experienced extensive fractional crystallization in a deep magma chamber and negligible crustal contamination during their ascent. Regarding the Palaeozoic tectonic development of the North Qilian orogenic belt, we propose that the Early Devonian lamprophyres and diorites possibly are related to North Qilian orogen unrooting and collapse and marking the end of the North Qilian orogenic events. |
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| Keywords: | North Qilian orogenic belt Alxa block Lamprophyres and diorites Petrogenesis Sr-Nd-Pb-Hf isotopes |
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