EPR 9-10°N热液烟囱体的结构特征与生长历史   总被引：1，自引：0，他引：1  

彭晓彤  周怀阳 《中国科学D辑》2005,35(8):720-728

对Alvin深潜器采集的4个EPR9-10°N热液烟囱体样品进行了结构和矿物地球化学研究,建立了不同烟囱体的形成环境和生长历史. EPR9-10°N热液烟囱体在形态、结构和组成上的差异, 反映了不同的两类热液沉积环境: 类型Ⅰ烟囱体形成于高温、较强酸性、强还原性热液集中流环境, 类型Ⅱ烟囱体则形成于相对低温、较弱酸性、富锌的还原性热液环境. 类型Ⅰ烟囱体的生长始于硬石膏的形成, 在此基础上, Cu-Fe-Zn硫化物在烟囱内各方向上的交代和沉淀过程决定了类型Ⅰ烟囱体的最终结构. 早期、中期、晚期硫化物形成阶段的建立恢复了类型Ⅰ烟囱体形成过程中温度变化和化学反应变化的历史. 与类型Ⅰ烟囱体不同, 类型Ⅱ烟囱体早期黄铁矿淬火结晶和闪锌矿结晶为烟囱体的生长提供了基础.  相似文献   

华南中侏罗世玄武岩的岩石地球化学研究--以福建藩坑玄武岩为例     

周金城  蒋少涌  王孝磊  杨竞红  张孟群 《中国科学D辑》2005,35(10)

华南发育一条近EW向展布的中侏罗世火山岩带, 福建永定盆地的"藩坑组玄武岩"是其中的典型代表之一. 藩坑玄武岩的TiO2为1.92 ～ 3.21 wt%, 属"高Ti玄武岩", 并有较高的全铁含量(11.09 wt%). 该玄武岩与东南沿海来自富集的岩石圈地幔的早白垩世玄武岩相比, 有完全不同的岩石地球化学特征: 相对富集Th, Nb, Ta, Zr和Ti等高场强元素, Zr/Ba, La/Nb, La/Ta, Zr/Y, Ti/Y, Ba/Nb, K/Ti和Rb/Zr等比值也与OIB相似; 除少数样品有较高εNd (T ) (1.87 ～ 3.55)外, 多数样品有类似球粒陨石的εNd (T)(-0.70 ～ 0.24), 属软流圈地幔来源并记录着软流圈与岩石圈相互作用的信息. 赣南、粤北、湘东南的(早-)中侏罗世玄武岩、辉长岩与福建藩坑玄武岩有相似的OIB型岩石地球化学特征. 这种OIB型玄武岩可作为该地区早中生代时期软流圈地幔上涌的岩石学标志. 软流圈地幔的上涌导致该地区构造伸展、裂谷盆地的形成.  相似文献   

湖南千里山-大义山-九嶷山成矿金三角的控矿意义     

陈庆  徐惠长  何周虎  黄革非 《华南地质与矿产》2005,(1):31-36,46

在综合前人资料的基础上，结合千里山-大义山-九嶷山地区典型矿区的实际调查，以矿床成矿系列理论为指导，根据壳源改造型和壳幔混熔型两类不同性质花岗岩(包括过渡产物)分异演化活动的成岩成矿规律以及矿源层与成矿的关系，揭示了本区成矿物质在区域地质构造不断演化过程中的行为，即成矿物质组合的变化、分散或富集规律，指出该地区今后地质找矿的六个重点区域。  相似文献   

河南内乡-淅川-带的虎睛石矿床及开发利用     

刘国范  杨振军李铭 马庚杰 《华南地质与矿产》2005,(1):68-71

研究区虎睛石矿床在地质特征、矿物组合、化学成分及琢雕效果等方面与国外虎睛石矿床是完全不同的，属于一种特殊的罕见类型。在分析虎睛石地质特征、开发利用现状的基础上，认为该区的虎睛石资源丰富，琢雕效果好，在国内外市场上具有一定的竞争力和良好的开发利用前景。  相似文献   

桩底注浆钻孔灌注桩承载力的研究     

李连营  林波  邵建 《岩土工程技术》2005,19(1):24-27

通过天津地区几例钻孔灌注桩桩底注浆的静载荷试桩结果 ,分析天津地区钻孔灌注桩桩底注浆单桩竖向极限承载力标准值的估算方法  相似文献   

云南省祥(云)-临(沧)公路红土坡隧道变形原因及加固方案     

邓星理  张翔杰 《中国地质灾害与防治学报》2005,16(2):74-79

云南省祥(云)-临(沧)公路红土坡隧道，在施工过程中变形严重，洞内数次冒顶、产生地面陷落，并诱发滑坡，严重影响了施工进度并造成较大经济损失。文章根据现场勘查及变形监控量测资料，详细论述了隧道变形特点，从地层岩性、构造、地应力条件、地下水作用、施工工艺、滑坡影响等方面综合分析了隧道变形原因。红土坡隧道变形是软弱的地层岩性、地应力条件改变、地下水作用、施工工艺以及滑坡偏压等各种因素共同作用的结果。且隧道变形诱发滑坡，滑坡又促使隧道进一步变形。基于此，文章提出了首先对滑坡进行支挡，再对隧道围岩进行加固的整治思路，并提出具体工程方案。整治工程实施后，红土坡隧道变形已得到完全控制，取得良好的治理效果。  相似文献   

上海市公共卫生中心空调设计     

寿炜炜  宋静  朱学锦 《中国勘察设计》2005,(8):34-37

介绍了上海市公共卫生中心空调通风的设计特点,突出反映在呼吸道传染病区、呼吸道门诊、呼吸道临检、生物安全实验室的系统设计中,并介绍了空调水系统的特殊要求。  相似文献   

GEOCHEMICAL CHARACTERISTICS OF PLATINUM GROUP ELEMENTS IN JINCHUAN SUPER-LARGE SULFIDE COPPER-NICKEL DEPOSIT, JINCHANG CITY, GANSU PROVINCE, CHINA     

WANG Ruiting MAO Jingwen HE Ying WANG Dongsheng TANG Zhongli 《大地构造与成矿学(英文版)》2005,29(2):152-163

The platinum-group element geochemistry of rocks and ores from Jinchuan super-large copper-nickel sulfide deposit is systemically studied in this paper. The Cu/Pd mean ratio of Jinchuan intrusion is lower than that of original mantle magma, which indicates that these ultrabasic rocks were crystallized from magma that lost Pd in the form of melting segregation of sulfides. The PGE of the rocks show trend of partial melting, similar to that of mantle peridotite, which shows that magma formation occurs during rock-forming and ore-forming processes. The chondrite normalized PGE patterns of the rocks and ores are well related to each other, which signifies the signatures of multi-episode magmatic intrusion, melting and differentiation in the formation processes of rocks and ores. In addition, analyses about the relation between PGE and S, and study on Re-Os isotopes indicate that few contamination of the crustal substances occurred during the magmatic intrusion and the formation of deposit. However, contamination by crustal substances helps to supply part of the S for the enrichment of PGE. Meanwhile, the hydrothermal process is also advantageous for the enrichment of PGE, especially lbr Pt and Pd, due to deep melting segregation. The characteristic parameters （such as Pt/（Pt＋Pd）, （Pt＋Pd）/（Ru＋Ir＋Os）, Pd/Ir, Cu/（Ni＋Cu）, and so on.） for platinum-group elements for Jinchuan sulfide copper-nickel deposit show the same features as those for sulfide copper-nickel deposit related to basic magma, which also illustrates its original magma property representative of Mg-high tholeiite. Therefore, it is the marie （not ultramafic） magma that resulted in the formation of the superlarge sulfide copper-nickel deposit enriched in Cu and PGE. To sum up, the geochemical characteristics of platinum-group elements in rocks and ores from Jinchuan copper-nickel sulfide deposit are constrained by the continental rift tectonic environment, the parent magma features, the enriched mantel magma source, the complex metallogenesis and PGE geochemical signatures, and this would be rather significant for the study about the genetic mechanism of copper-nickel sulfide deposits.  相似文献   

Ruthenium-ion-catalyzed oxidation of asphaltenes and oil-source correlation of heavy oils from the Lunnan and Tahe oilfields in the Tarim Basin, NW China     

马安来张水昌  张大江金之钧马晓娟  陈清棠 《中国地球化学学报》2005,24(1):28-36

The identification of marine source rocks in the Tarim Basin is debated vigorously. The intention of this paper is to investigate the asphahenes in heavy oils from the Lunnan and Tabe oilfields and Well TD2 with ruthenium-ions-catalyzed oxidation technique (RICO), in order to explore its role in oil-oil and oil-source correlations, The RICO products included n-alkanoic acids, α,ω-di-n-alkanoic acids, branched alkanoic acids, tricyclic terpanoic acids, hopanoic acids, gammacerane carboxylic acid , regular sterane carboxylic acids and 4-methylsterane carboxylic acids. The n-alkyl chains and biomarkers bounded on the asphaltenes were of unsusceptibility to biodegradation. The distribution and absolute concentrations of n-alkanoic acids in the RICO products of heavy oils from the Lunnan and Tabe oilfields are different from those of Well TD2. The biomarkers bounded on the asphahenes, especially steranes, have a distribution trend similar to that of the counterparts in saturates. The sterane carboxylic acids and 4-methylsterane carboxylic acids in the RICO products of heavy oils from the Lunnan and Tahe oilfields, dominated by C30 sterane and C31 4-methylsterane carboxylic acids, respectively, are significantly different from those of the heavy oils of Well TD2, whose dominating sterane and 4-methylsterane carboxylic acids are C28 sterane and C29 4-methylsterane acids, respectively. The RICO products of the asphaltenes further indicate that the Middle-Upper Ordovician may be the main source rocks for heavy oils from the Lunnan and Tabe oilfields.  相似文献   

燕辽造山带东段中、新生代构造演化的盆地沉积物热年代学记录     

闫义  林舸  夏斌  李自安  李忠诚 《地质学报》2005,79(2):286

盆地碎屑沉积物单颗粒低温磷灰石裂变径迹年龄与高温锆石U-Pb年龄相结合 ,可以更好地示踪盆地沉积物源区构造 -热事件信息及沉积后盆地热演化历史。辽西北票盆地中生代沉积物碎屑锆石U-Pb年龄大部分落入 194.3± 2 .9Ma至 2 3 3 .8± 4.2 Ma范围内 ,大多数碎屑磷灰石颗粒裂变径  相似文献