Petrology, geochemistry and ore mineralization of anorogenic granitoids of shibelikskii complex in Gorny Altai
The relevance of the discussed issue is caused by the need of researching petrology, geochemistry and ore mineralization of anorogenic granitoids of Shibelikskii complex which is represented by strong fractionated rocks. Different types of ore mineralization of Zr, Nb, Ta and REE are related to such...
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| Format: | Article |
| Language: | Russian |
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Tomsk Polytechnic University
2016-08-01
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| Series: | Известия Томского политехнического университета: Инжиниринг георесурсов |
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| Online Access: | http://izvestiya-tpu.ru/archive/article/view/1766 |
| Summary: | The relevance of the discussed issue is caused by the need of researching petrology, geochemistry and ore mineralization of anorogenic granitoids of Shibelikskii complex which is represented by strong fractionated rocks. Different types of ore mineralization of Zr, Nb, Ta and REE are related to such rocks spatially and paragenetically. The main aim of the research is to study petrology, geochemical features of rocks, accessory mineral zircon and ore mineralization of Shibelikskii areal using the experimental diagrams, which allow revealing the genetic problems and determining physic-chemical features of magamatic and hydrothermal zircon crystals. The methods used in the study. Rare and scattered elements were determined in rocks by inductively coupled plasma method on the mass spectrometer «ОРTIMA-4300», the rest elements, including REE, were determined by La-ISP-MS methods in the Laboratory OIGaG SO RAN (Novosibirsk). Chemical elements in zircon were determined by La-ISP-MS mass-spectrometry method with inductively coupled plasma and laser ablation on the mass-spectrometer ELEMENT 2 (Thermo Finnigan Mat) with laser device UP-2B, Nd: YAG (New Wave Research) in the Laboratory OIGaG SO RAN (Novosibirsk). Results. The paper introduces the data on geochemistry and petrology of alkali granitoids and accessory magmatic and hydrothermal zircon of Shibelikskii complex in Gorny Altai. Based on the representative analysis of rocks and zircon the features of granitoids generation, their ore mineralization and typification are determined. The granitoids refer to agpaitic strong fractionation rocks. The tetradic effect of REE M-type fractionation appears in the rocks and in zircon. It is caused by high saturation with fluoro-rich fluids. Increase in meanings of tetradic effect of REE is correlated with the growth of the environment acidity. The author has determined the extreme non-coherence of elements ratio to chondrite and non-conformity of behavior to charge-and-radius-controlled characteristics. Magmatic zircon is characterized by prismatic and pyramid crystal form and high contents of Hf, Y, Sc, and heavy REE. Hydrothermal zircon has higher contents of Nb, Ta and sum of REE. |
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| ISSN: | 2500-1019 2413-1830 |