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Geochemistry of the Cenozoic Potassic Volcanic Rocks in the West Kunlun Mountains and Constraints on Their Sources

Acta Geologica Sinica(English Edition) 2004年第4期78卷 912-920页

作者： zhangzhaochong XIAOXuchang WANGJun WANGYong LUOZhaohua InstituteofGeology ChineseAcademyofGeologicalSciencesBeijing100037 InstituteofGeology ChineseAcademyofGeologicalSciencesBeijing100037／／ChinaUniversityofGeosciencesBeijing100087 ChinaUniversityofGeosciences Beijing100087

The geochemical characteristics of the Cenozoic volcanic rocks from the north Pulu, east Pulu and Dahongliutan regions in the west Kunlun Mountains are somewhat similar as a whole. However, the volcanic rocks from the Dahongliutan region in the south belt are geochemically distinguished from those in the Pulu region (including the north and east Pulu) of the north belt. The volcanic rocks of the Dahongliutan region are characterized by relatively low TiO2 abundance, but more enrichment in alkali, much more enrichment in light rare earth elements and large ion lithosphile elements than those from the Pulu region. Compared with the Pulu region, volcanic rocks from the Dahongliutan region have relatively low 87Sr/86Sr ratios, and high εNd, 207Pb/204Pb and 208Pb/204Pb. Their trace elements and isotopic data suggest that they were derived from lithospheric mantle, consisting of biotite- and hornblende-bearing garnet lherzolite, which had undertaken metasomatism and enrichment. On the primitive mantle-normalized patterns, they display remarkably negative Nb and Ta anomalies, indicating the presence of early-stage subducted oceanic crust. The metasomatism and enrichment resulted from the fluid released from the crustal materials enclosed in the source region in response to the uplift of asthenospheric mantle. Based on the previous experiments it can be inferred that the thickness of the lithosphere ranges from 75 to 100 km prior to the generation of the magmas. However, the south belt differs from the north one by its thicker lithosphere and lower degree of partial melting. The different thickness of the lithosphere gives rise to corresponding variation of the degree of crustal contamination. The volcanic rocks in the south belt are much more influenced by crustal contamination. In view of the tectonic setting, the generation of potassic magmas is linked with the uplift of asthenosphere resulted from large-scale thinning of the lithosphere after the collision of Indian and

关键词： potassic magma lithospheric mantle asthenospheric mantle metasomatism west Kunlun Mountains

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Petrology, Mineralogy and Geochemistry of the Emeishan Continental Flood Basalts, SW China: Evidence for Activity of Mantle Plumes

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Acta Geologica Sinica(English Edition) 2004年第1期78卷 40-51页

作者： zhangzhaochong HAOYanli WANGFusheng JohnJ.MAHONEY InstituteofGeology ChineseAcademyofGeologicalSciencesBeijing100037China SchoolofOceanandEarthScienceandTechnology UniversityofHawaiiHonoluluHI96822USA

Electronic microprobe analyses for olivine, clinopyroxene and Cr-spinel in picrites, which we have discovered recently in the Emeishan continental flood basalt province (ECFBP), show that the olivine is rich in Mg, and that Cr-spinel is rich in Cr. Based on the olivine-melt equilibrium, the primary parental melt compositions are calculated. The high-Mg olivine-hosted picrite can be regarded as parental melt. Thus, the melting temperature and pressure are estimated: T=1600℃ and P=4.5 GPa. It suggests that the picrites are connected with the activity of mantle plumes. Their major element composition is comparable to many other CFBs by their high Fe8, (CaO/Al2O3)8 and low Na8, indicating a high pressure. All rocks display a similar chondrite-normalized REE patterns, i.e., enrichment of LREE, relative depletion of HFSE and absence of negative Nb and Ta but depletion in P and K. Some incompatible element ratios, such as La/Ta, La/ Sm, (La/Nb)PM, (Th/Ta)PM, are in a limited range, show that they were derived from the mantle plume, and there was no or little crustal contamination during magma ascent en route to the surface. They were generated by 7% partial melting of garnet peridotite. The axis of the plume might be located beneath Lijiang Town, Yunnan province.

关键词： continental flood basalts picrite geochemistry Emeishan

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Middle Devonian Picrites of the Southern Margin of Altay Orogenic Belt and Implications for the Tectonic Setting and Petrogenesis

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Journal of China University of Geosciences 2005年第2期16卷 95-103页

作者： zhangzhaochong YanShenghao ChenBailin ZhouGang HeYongkang ChaiFengmei HeLixin State Key Laboratory of Geological Processes and Mineral Resources.China University of Geosciences Beijing 100083China Institute of Mineral Resources.Chinese Academy of Geological Sciences Beijing 100037.China Institute of Geomechanics Chinese Academy of Geological Sciences.Beijing 100081.China No.4 Geological Party Xinjiang Bureau of Geology and ResourcesAltay 836500.China

The Altay orogenic belt of Xinjiang in NW China represents one of the important sites of juvenile crustal growth during the Phanerozoic. However, some important issues, e.g., tectonic evolution and petrogenesis, still remain controversial. The picrites in the south margin of the Altay orogenic belt were discovered in the lower part of marine volcanic-sedimentary sequences of the northwest-striking Middle Devonian Beitashan Formation (Fm.), which consists chiefly of intermediate-basic volcanic rocks intercalated minor carbonate, siltstone and siliceous rocks. The picrites are usually highly porphyritic, and contain abundant forsteritic olivine phenocrysts with minor clinopyroxene distributed in the groundmass, which consist of olivine, clinopyroxene and plagioclase with minor Fe-Ti oxides. The MgO contents of the picrites range from 14 wt% to 22 wt% with Mg# (atomic Mg/(Mg+Fe) ratio) of 0.75-0.80. They are characterized by slightly negative Ti anomalies, remarkably negative Nb and Ta anomalies and slightly positive P and Sm anomalies with the similar abundances of HFSE as MORB on the MORB-normalized trace element patterns, all of which characterize typical island arc magmas. In combing with the southwestward migration of the magmas of the Beitashan Fm., we propose that the magmas may result from the southwestward subduction of Junggar ocean plate. The Zr/Nb ratios (23-66) of both picrites and basalts resemble the MORB (10-66), suggesting that they were derived from the MORB-like sources. However, the basalts and picrites display some distinguishable element ratios and REE patterns, e.g., Ti/V (23-35) and Zr/Sm (18-23) ratios of basalts are higher than those of picrites (14-17 and 14-15 respectively), and the basalts display flat-type REE-chondrite patterns whereas the picrites are characterized by lower total REE concentrations ((26-34)×10^-6) and slight enrichment of light REE. These distinguished geochemical characteristics could be interpreted by different partial

关键词： picrite geochemistry island arc,Middle Devonian,Altay orogenic belt

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内蒙古迪彦钦阿木超大型钼矿床成矿流体特征及成矿机制

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岩石学报 2018年第12期34卷 3582-3596页

作者：王瑞良张招崇曾庆栋王永彬郭祺褚惠燕郭云鹏郭理想中国地质大学地球科学与资源学院北京100083 中国科学院地质与地球物理研究所中国科学院矿产资源研究重点实验室北京100029 中国科学院地球科学研究院北京100029 中国科学院大学北京100049

迪彦钦阿木钼矿是近年来发现的一个超大型斑岩钼矿床,位于大兴安岭中段二连浩特-东乌旗多金属成矿带。本文主要对迪彦钦阿木钼矿床的流体包裹体及硫同位素进行了系统研究。迪彦钦阿木钼矿发育有四个成矿阶段:石英-钾长石阶段、石英-辉... 详细信息

迪彦钦阿木钼矿是近年来发现的一个超大型斑岩钼矿床,位于大兴安岭中段二连浩特-东乌旗多金属成矿带。本文主要对迪彦钦阿木钼矿床的流体包裹体及硫同位素进行了系统研究。迪彦钦阿木钼矿发育有四个成矿阶段:石英-钾长石阶段、石英-辉钼矿阶段、石英-多金属硫化物阶段及石英-萤石-碳酸盐阶段。矿床不同阶段的流体包裹体中,富气相(V类)、富液相(L类)和含子晶(S类)包裹体大量共存。显微测温结果显示,第一阶段包裹体均一温度为492～> 600℃,盐度分为两部分:5. 36%NaCleqv(L类)和32. 39%～64. 90%NaCleqv(S类);第二阶段包裹体均一温度为292～510℃,盐度为4. 49%～19. 92%NaCleqv(L类)和28. 43%～70. 21%NaCleqv (S类);第三阶段包裹体均一温度为206～388℃,盐度为2. 24%～22. 71%NaCleqv(L类)和28. 62%～54. 64%NaCleqv(S类);第四阶段包裹体均一温度、盐度最低,均一温度为133～288℃,盐度为0. 88%～7. 86%NaCleqv。流体具有从高温、高盐度向低温低盐度演化趋势。前三个成矿阶段L类、V类和S类包裹体大量共存,端元包裹体均一温度相近,盐度相差很大,表明发生了强烈的流体沸腾作用。多期次的流体沸腾作用是迪彦钦阿木矿床的主要成矿机制。硫同位素研究显示,δ^(34)S值的变化范围是1. 78‰～10. 41‰,暗示着迪彦钦阿木钼矿成矿物质主要来自于岩浆。

关键词：流体包裹体硫同位素超大型斑岩钼矿床迪彦钦阿木大兴安岭

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