Ore Genesis and Formation Age of the Gaogangshan Mo Deposit,Heilongjiang Province,NE China

The Gaogangshan Mo deposit, located in the northern part of the Lesser Xing'an Range (the eastern part of the Xing'an–Mongolia Orogenic Belt), is one of the newly discovered Mo deposits in northeast China. Ore bodies occur in the granite and are generally in vein and stockwork forms. Major metallic minerals in the ore include pyrite and molybdenite. The styles of mineralization are disseminated, veinlet–disseminated, and veinlet. The major types of wall–rock alteration are silicification–potassic alteration, phyllic alteration and propylitization. Fluid inclusion analyses indicate that the ore‐forming fluid during the major mineralization stage is an H₂O–NaCl–CO₂ system, with wide homogenization temperature and salinity ranges. The abundant CO₂–rich and coexisting halite–bearing fluid inclusion assemblages in the main stage of mineralization highlight the significance of intensive fluid boiling for porphyry Mo mineralization. Comprehensive study of the ore‐forming conditions, geological features of the deposit, micro‐thermometric analysis of fluid inclusions and comparison of the Gaogangshan deposit with other typical porphyry deposits leads to the conclusion that the deposit is a porphyry type. We obtained a weighted mean age of the molybdenite deposit at Gaogangshan of 250.7 ± 1.8 Ma. The isotopic dating results indicate that the Gaogangshan deposit was formed in the Permo–Triassic, which is the earliest Mo–only deposit in northeast China. The formation of the Gaogangshan Mo deposit may be related to the extension and break–up of the Songnen Block and Jiamusi Block in the Permo–Triassic.     

北秦岭松树沟榴辉岩的确定及其地质意义

松树沟石榴石角闪岩(榴闪岩)呈透镜状产于松树沟超镁铁岩旁侧的斜长角闪岩中,一直以来被认为是形成于接触交代变质或麻粒岩相变质过程。详细岩相学及矿物元素分析,在榴闪岩的基质矿物、石榴石幔部及锆石包体中发现残留的绿辉石,而且石榴石也保存了明显的进变质主、微量元素成分环带,表明松树沟榴闪岩为榴辉岩退变质的产物,至少经历了从角闪岩相到榴辉岩相再到角闪岩相的三阶段顺时针PT演化过程。锆石定年结果得到榴辉岩的变质年龄为500±8Ma,原岩结晶时代为796±16Ma,与秦岭岩群北侧官坡超高压榴辉岩的变质年龄和原岩年龄完全一致,也与北秦岭区域高压-超高压变质时代和原岩的结晶时代一致。表明松树沟榴辉岩与北秦岭造山带已发现的高压-超高压变质岩石一起都应是古生代大陆深俯冲作用的结果,而松树沟超镁铁岩可能是俯冲的大陆板片在折返过程中携带的俯冲隧道中的交代地幔岩。     

Research on Biofacies their Provincialization of Middle Permian-MiddleTriassic in the western Sichuan Basin

The research area is located in the western part of Sichuan basin as a Yangtze ecotope of Cathaysian Tethyan area. It is dominated by benthic fauna, including brachiopods, Fusulinids, corals, bivalves, foraminifers, ammonites, bryozoans, Crinoids and pleopods are less common with traces of trilobites, stromatoporas, nautilus and sporopollens seen in one or two areas,which are obviously controlled by sedimentary environments in accordance with sedimentary facies. On the basis of division and research of biological communities and according to the combination of communities with sedimentary characteristics, six kinds of biofacies have been recognized and described in the study area,i.e. benthic biofacies of restricted platform, benthic biofacies of open platform, benthic biofacies of inner gentle slope, benthic biofacies of outer gentle slope, benthic biofacies of shelf slope and swimming biofacies of deep-water basin. Based on the study of middle Permian to middle Triassic biofacies,biofacies pattern are established, category, ecotype, typical community, sedimentary facies and oil bearing of each biofacies are elucidated in this paper. According to the association law of biofacies in time and space, the ahthors think that there are three biofacies provinces in the study area, i.e., platform biofacies province, slope biofacies province and basin biofacies province.The distribution characteristics of bioface types indicates that the platform-type and ramp-type biofacies are mainly distributed in the subject of the study area. It indicates that their distribution are mainly controlled by Yangtze platform. But the bioface of deep water basin type biofacies and basin biofacies province are mainly distributed at the edge of study area, indicating that they are mainly controlled by the Longmen trough. The study of biofacies and their provincialization of Middle Permain-Middle Triassic in the Western Sichuan Basin is a reference for the reconstruction of paleogeography and paleo-plate.Therefore, the research is meaningful for the analysis of paleogeography, tectonics and their evoulution of the Sichuan Basin.     

基于Archimedean Copula函数的风浪联合统计分析

选取渤海海域某导管架平台24年的年最大波高和相应风速,基于Gumbel分布对2个边缘分布的拟合优度检验,采用Archimedean Copula函数族中的4种函数构建两变量联合概率分布模型,并进行了拟合优度评价。利用优选出的Clayton Copula函数,计算风浪联合分布的联合重现值。以海洋平台响应作为约束条件,进行了二维Clayton Copula函数的风浪联合统计分析。研究结果表明:基于Copula函数构造的二维分布,考虑了风浪之间的相关性,在相同重现值设计参数下,可以降低导管架平台的结构响应,从而可以降低海洋平台的环境条件设计标准。     

白令海和楚科奇海表层沉积物中多环芳烃降解微生物多样性

为了研究白令海(海盆及陆架)至楚科奇海陆架表层沉积物中多环芳烃(PAHs)降解菌的多样性,并获得新的PAHs降解菌资源。在GC-MS分析沉积物中PAHs种类和含量的基础上,以萘、菲和芘的混合物为唯一碳源和能源对表层沉积物样品进行富集,通过平板分离鉴定可培养菌株,并验证其降解能力;同时利用变性梯度凝胶电泳(DGGE)和Illumina高通量测序技术分析降解菌群结构。GC-MS测定结果表明,14个表层沉积物中PAHs总干质量介于32.99~276.97ng/g。富集菌群中共分离获得51株可培养细菌,平板纯培养、PCR-DGGE及Illumina测序结果均表明,菌群中优势的降解菌是γ-proteobacteria的Marinobacter,Pseudoalteromonas,Pseudomonas和Actinobacteria门的Dietzia菌。此外,Illumina测序结果还表明14个降解菌群在菌群结构组成上,可分为海盆区和陆架区两种类群;同时检测到一些低丰度的海洋专属PAHs降解菌,如Cycloclasticus,Alteromonas和Neptunomonas等。本文结果将加深对白令海及楚科奇海表层沉积物中PAHs降解菌资源与生物多样性的认识。     

分布式异构警用地理信息平台设计和联网实现

公安部门跨部门、跨区域的警务协作,要求实现全国范围内地理信息的分布式访问。本文描述了在建设全国警用地理信息平台时,依托公安专用网络环境中,基于各地所采用的异构基础GIS平台,设计和实现多节点分布式警用地理信息平台的策略、方法和算法,并介绍了相关的标准规范、系统安全、运维监控等平台支撑技术。     

HJ-1卫星CCD数据的大气校正及其效果分析

利用MODTRAN 4模型对地表-大气-遥感器之间的辐射传输过程进行模拟,模拟出对应大气参数下的表观辐亮度;利用模拟生成的大气校正查找表,逐像元对HJ-1卫星CCD数据进行大气校正;并从光谱曲线、与MODIS地表反射率产品比较、归一化植被指数(NDVI)三个方面,探讨了HJ-1卫星CCD数据大气校正效果.结果表明:(1...     

中国北方不同气候区晴天陆面过程区域特征差异

采用2008年7～9月份观测的中国干旱-半干旱区实验观测协同与集成研究资料,将我国北方干旱一半干旱区根据气候类型和地理位置划分为西北干旱区、黄土高原区和东北冷区三个区域,分析了干旱-半干旱区陆面热量平衡和辐射平衡日变化的区域差异.结果显示:不同气候区域的地表辐射和能量过程差异明显,而这种差异主要源于大气和土壤中可利用水...