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| 1 | 塔里木早二叠世大火成岩省的时空特征和岩浆动力学显示文摘塔里木早二叠世大火成岩省是继峨眉山大火成岩省之后在中国境内发现的又一个二叠纪大火成岩省。近十多年来,对塔里木大火成岩省及其与地幔柱和大规模成矿的关系受到极大关注。本文结合近年来国内外的最新研究进展,对塔里木大火成岩省的时空分布、岩石地球化学特征、成因演化和动力学过程以及成矿潜力进行综述。塔里木大火成岩省的残余分布面积达25万km2,岩石类型主要有大陆溢流玄武岩(分布广泛),长英质火山岩类(主要分布在塔里木盆地的北部)和基性-超基性及中酸性侵入岩类等(主要出露于巴楚、巴什索贡和皮羌等地区)。该大火成岩省事件的岩浆活动时间主要集中在292~285 Ma(玄武岩和第一期长英质火山岩类形成阶段)和284~274 Ma(侵入岩类、含钒钛磁铁矿床和第二期长英质火山岩类形成阶段)。系统和深入的岩石地球化学和Sr-Nd-Hf-Pb同位素研究表明,塔里木大火成岩省从早期喷发的玄武岩到晚期的侵入岩类具有明显不同的地球化学特征,指示其岩浆源区发生了从富集岩石圈地幔来源到地幔柱来源的明显转变。结合相关的地质学和岩石学证据及铂族元素(PGEs)等研究,提出了一个上涌的地幔柱不断向位于岩石圈地幔底部的岩浆源区注入亏损地幔物质、持续改变其同位素地球化学特征并最终形成塔里木大火成岩省各主要岩石类型的岩浆演化新模型。最后,巴楚瓦吉里塔格含钒钛磁铁矿的存在也表明在塔里木大火成岩省中具有找寻大型钒钛磁铁矿床的潜力。 | 厉子龙 励音骐 邹思远 孙浩伟 李东旭 | 2017 | 矿物岩石地球化学通报2017，36，3： | 10 |
| 2 | Application of Stable Strontium Isotope Geochemistry and Fluid Inclusion Microthermometry to Studies of Dolomitization of the Deeply Buried Cambrian Carbonate Successions in West-Central Tarim Basin, NW China显示文摘Detailed petrographic,geochemical(O-C-Sr isotopes)and fluid inclusion studies of the deeply buried Cambrian carbonates in the West-central Tarim Basin revealed three types of crystalline dolomites(fine-crystalline,nonplanar-a(s),dolomite(RD1),fine-to medium-crystalline,planar-e(s)dolomite(RD2),and medium-to coarse-crystalline,nonplanar-a dolomite(RD3)),medium-to coarsecrystalline,nonplanar-a saddle dolomite cement(CD)and early and later-stage calcite cement.The occurrence of RD1 along low-amplitude stylolites points to link with pressure dissolution by which minor Mg ions were likely released for replacive dolomitization during early-to intermediate-burial seawater dolomitization.The increasing crystal sizes of RD2 and RD3 with irregular overgrowth rims suggests intense recrystallization and replacement upon the RD1 or remaining precursor limestones by dolomitizing fluids during late intermediate burial dolomitization.The overlap ofδ^(18)O,δ^(13)C and ^(87)Sr/^(86)Sr values of RD1-RD3 and CD dolomite with coeval seawater values,suggests that the principal dolomitizing fluids that precipitated these dolomites was connate(Cambrian)seawater preserved in the host limestones/dolomites.Their high ^(87)Sr/^(86)Sr ratios suggest influx of radiogenic strontium into the Cambrian seawater.Two regimes of fluid flow are recognized in the study area:firstly,influx of magnesium-rich higher-temperature basinal brines along deep-seated faults/fractures,resulting in cementation by CD dolomite.Secondly,the incursion of meteoric waters,mixing with ascending highertemperature basinal brines,and an increase in Ca^(2+)/Mg^(2+)ratio in the fluids probably results in the precipitation of calcite cement in vugs and fractures. | Ngong Roger Ngia Mingyi Hu Da Gao Zhonggui Hu Chun-Yan Sun | 2019 | Journal of Earth Science2019，30，1： | 5 |
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