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901.
贵池铜山岩体岩石化学与地球化学特征 总被引:4,自引:0,他引:4
通过岩石化学、微量元素地球化学、稀土元素地球化学、铅同位素地球化学特征研究表明, 铜山石英闪长岩、花岗闪长岩、二长花岗岩是同一岩浆源同一时期( 燕山早期) 三个侵入阶段的产物, 铜山岩体幔壳同熔型的复式岩体, 属太平洋钙碱性岩石系列。铜山铜矿床的形成与铜山复式岩体的岩浆充分演化分异有关。 相似文献
902.
903.
The paper reviews data (acquired in 2007–2016) on aliphatic and polycyclic aromatic hydrocarbons in comparison with data on concentrations of lipids, Corg, and chlorophyll a in the water and bottom sediments the river–sea geochemical barrier (for the Northern Dvina, Ob, Yenisei, and Lena rivers). It was established that the concentrations of anthropogenic hydrocarbons decrease and these compounds precipitate like other organic compounds and particulate matter, where riverine and marine waters mix. Relatively pure water flows in the pelagic zones of seas. In spite of low temperatures in the Arctic, anthropogenic hydrocarbons transform so rapidly that natural compounds dominate in the water and bottom sediments: autochthonous in the seawater and allochthonous in the bottom sediments. 相似文献
904.
N. A. Nekrylov D. V. Popov P. Yu. Plechov V. D. Shcherbakov L. V. Danyushevsky O. V. Dirksen 《Petrology》2018,26(4):329-350
Late Quaternary volcanoes of Sredinny Range (Kamchatka) attract geoscientists’ attention by their unusual geochemical features and geodynamic setting. They produced volcanic rocks that are enriched relative to N-MORB in most of incompatible trace elements (except HREE), including strong enrichment in large-ion lithophile elements, and show a negative Nb–Ta anomaly, which is typical for rocks formed in supra-subduction settings. However, modern subduction of the Pacific Plate does not reach the most part of Sredinny Range, as inferred by mapping of Wadati–Benioff zone or seismic tomography. We constrain the source of parental magmas for Sredinny Range volcanic rocks by combining major and trace element geochemical data for olivine and naturally quenched olivine-hosed melt inclusions for Holocene tephra layers of the Kekuknaisky field. Composition of the most magnesian olivine (Ni > 2000 ppm, Fe/Mn ≈ 75 at Mg# ~ 84–85 mol %) and geochemical characteristics of the most primitive melts (FC3MS = 0.61 ± 0.04 (2s)) are consistent with their derivation from a pyroxenite source, while elevated LREE/HREE ratios in lavas indicate that it contained garnet. This garnet-bearing pyroxenite likely originated from the lower crust or lithospheric mantle. Its melting could have occurred due to delamination and sinking into the hotter mantle. 相似文献
905.
V. Yu. Kuznetsov E. V. Tabuns G. A. Cherkashev V. E. Bel’tenev F. E. Maksimov K. A. Kuksa L. I. Lazareva S. B. Levchenkoa I. E. Zherebtsov 《Doklady Earth Sciences》2018,478(1):26-30
The results of 230Th/U dating and mineralogical–geochemical studies of sulfide ores from the Irinovskoe hydrothermal field and the Severo-Zapadnoe ore occurrence (Mid-Atlantic Ridge) are presented. Sulfides are represented primarily by copper–sulfide ores with 12–30% Cu content; sulfur- and zinc-sulfide ores are distributed less frequently. The analysis of a change in the composition of sulfides over time has made it possible to identify three stages of formation. Each stage assumes that mineral associations are changed from high-temperature (sulfur and copper sulfide) to medium temperature (Zn–Cu and Zn-sulfide) sulfide ores. The whole age range of formation of the hydrothermal deposits falls within the time interval of about 58000–8000 for the Irinovskoe field and 69000–11000 years ago for the Severo-Zapadnoe ore occurrence. 相似文献
906.
中国东北浅覆盖区地质填图物化探信息协同辅助技术 总被引:1,自引:0,他引:1
针对中国东北浅覆盖区地质露头少、填图效率不高、精确度和准确度较低的问题,开发了物化探信息协同辅助技术并应用于地质体类型的识别。在以覆盖层较薄、面积广大、物理风化为主、土壤位移较小为特点的东北森林沼泽浅覆盖区,利用土壤化学成分和航磁信息识别下伏地质体是可行的。基于这一前提,可将指定研究区划分为一定数量的统计单元,在各单元内,通过数学统计方法产生众数、宽度、变化频率、偏度、峰度等航磁特征参数并将其标准化,将化探指标酸度、碱度、钙含量、铝含量、钙镁含量、硅铝含量、镁铁含量、微量元素含量等特征参数标准化;然后采用逐级分类的方法,每级选择有效的物化探特征参数,在当前级别上实现单元划分并将数据分为不同数据集,在下一级别划分时重新有针对地选择参数,分别对各数据集进一步分类,直到分类结果对应较明确的地质填图单元,并最终编制出解译图。以黑龙江省大兴安岭地区某典型森林沼泽浅覆盖区为例进行了方法验证,将结果与已知地质信息比对分析,认为地质体单元识别结果与已知信息基本吻合,使得地质体类型识别更精确,边界更清晰,可为区域地质研究提供新线索。 相似文献
907.
Yakovenchuk V. N. Pakhomovsky Ya. A. Konoplyova N. G. Panikorovskii T. L. Mikhailova Yu. A. Bocharov V. N. Krivovichev S. V. Ivanyuk G. Yu. 《Geology of Ore Deposits》2018,60(7):587-593
Geology of Ore Deposits - Epifanovite, NaCaCu5(PO4)4[AsO2(OH)2] · 7H2O, a new natural copper, sodium and calcium arsenate–phosphate, has been found in a quartz–phosphate pocket... 相似文献
908.
Yakovenchuk Victor N. Ivanyuk Gregory Yu. Pakhomovsky Yakov A. Panikorovskii Taras L. Britvin Sergei N. Krivovichev Sergey V. Shilovskikh Vladimir V. Bocharov Vladimir N. 《Mineralogy and Petrology》2018,112(1):111-121
Mineralogy and Petrology - Kampelite, Ba3Mg1.5Sc4(PO4)6(OH)3·4H2O, is a new Ba-Sc phosphate from the Kovdor phoscorite-carbonatite complex (Kola Peninsula, Russia). It is orthorhombic, Pnma,... 相似文献
909.
The effect of the structural irregularity of an interstellar cloud on the dynamics of its disruption by a shock from a supernova is studied. Irregular clouds are disrupted twice as fast as spherical clouds. However, fragments of irregular clouds preserve their enhanced density for long times without being mixed with the intercloud gas. The fraction of shock energy that is converted to the kinetic energy of the fragments is 50% higher than in the disruption of a spherical cloud. Shocks are not able to trigger the gravitational compression of clouds. 相似文献
910.
A. A. Kadik N. A. Kurovskaya O. A. Lukanin Yu. A. Ignat’ev V. V. Koltashev E. B. Kryukova V. G. Plotnichenko N. N. Kononkova 《Geochemistry International》2017,55(2):151-162
The contents and speciation of nitrogen, carbon, and hydrogen were determined in basalt–basaltic andesite melts in equilibrium with liquid Fe alloys at 1.5 Gpa, 1400°C, and oxygen fugacity (fO2) 1.4–1.9 log units below that of the Fe–FeO buffer (ΔlogfO2(IW) =–1.4 …–1.9). Experiments were carried out on a piston- cylinder type apparatus using welded Pt capsules in the presence of excess С (graphite). Starting mixture consisted of natural ferrobasaltic glass and silicon nitride (Si3N4) as nitrogen source in the system. Experimental quench products representing glasses with spherical inclusions of iron alloy were analyzed using electron microprobe, Raman, and IR spectroscopy. With increase of Si3N4 in the starting mixture and, respectively, decrease of fO2, silicate melt forming during experiments became depleted in FeO and enriched in SiO2. It was established that the nitrogen content in the glasses increases from 0.13 to 0.44 wt % with decrease of ΔlogfO2(IW) from–1.4 to–1.9, whereas C content in the first approximation remains constant within 1.18–1.13 wt %, while the total water content (ОН– + Н2О) determined by IR spectroscopy decreases from 4.91 to 1.20 wt %. The N (0.13–0.48 wt %) and C (0.75–2.26 wt %) contents determined in the Fe alloy show no clear correlation with fO2. The IR and Raman spectroscopic study of the glasses indicates the formation of molecules and complexes with bonds N–H (NH3, NH2 ?, NH2 +, NH4 +), Н–О (Н2О, OH–), С–Н (СН4) as well as N2 and Н2 molecules in silicate melts. IR spectra also reveal the presence of complexes with С=О, С–N bonds and СО2 molecules. Obtained data are compared with results of previous studies on the solubility and speciation of N, С, and Н in the model FeO–Na2O–SiO2–Al2O3 melts in equilibrium with liquid iron alloys at 1.5 GPa (1400°C) and 4 GPa (1550°C) (Kadik et al., 2011, 2015). 相似文献