锡氢化物是锡的重要迁移形式

论述了锡氢物的形成条件和物理学特征。在岩浆和热液中，锡以锡氢化物，锡合金氢化物迁移至地壳浅部，锡氢化物，锡合金氢化物被氧化成锡氧化物，锡合金矿物，或与硫，硫化氢作用形成锡的硫化矿物。     

宣城地区龙潭组页岩沉积环境与有机质富集

安徽宣城地区上二叠统龙潭组海陆过渡相页岩不仅是我国下扬子区重要的烃源岩,也是目前我国页岩气勘探的重要层位之一.为研究海陆过渡相页岩沉积环境与有机质富集的关系,以港地1井和两个露头剖面为研究对象,系统开展了有机地球化学测试、有机岩石学研究、氩离子抛光—扫面电镜观察、元素地球化学分析等工作.结果表明:下扬子宣城地区龙潭组页...     

基于计算流体力学的寒区土壤水热耦合模型研究

土壤水文过程(水分运移和传热)及其对气候变化的响应是寒区水文学的前沿问题.然而,冻土的存在使得寒区土壤水文过程变得极其复杂.此外,寒区自然环境恶劣,较难获取长时间序列和高分辨率的野外观测资料.近年来,充分利用已有的观测数据,构建寒区土壤水热耦合模型,并开展相应的数值模拟研究,已成为理解寒区土壤水文物理过程,揭示其动力学...     

辽西义县组与冀北大店子组、西瓜园组的对比

辽西义县组与冀北大店子组、西瓜园组的对比关系一直存有分歧.综合分析前人生物地层学资料,并结合同位素年代学,提出老公沟层、业南沟层、尖山沟层和冀北滦平盆地大店子组1~2段及3~4段下部相当,大康堡层可与大店子组3~4段上部对比,金刚山层与西瓜园组大致相当.     

A statistical analysis applied to the Rf/φ method

A statistical analysis for the R_f/φ method is developed in the paper. The technique provides estimates of R_s, R_i and θ according to R_f and φ. Moreover, we can restore the pattern of initial orientations of marker objects by means of their frequency histogram, provided the strain is homogeneous. It is unnecessary to postulate random initial orientations if the principal directions of strain ellipsoid are known.     

鄂尔多斯盆地东北部构造热演化史的磷灰石裂变径迹分析

运用磷灰石裂变径迹(AFT)分析的构造热年代学研究方法,系统探讨鄂尔多斯盆地东北部不同区段中新生代以来的热演化历史,为盆地东北部石油和天然气等多种沉积能源矿产的勘探预测提供新的约束条件。模拟结果表明:盆地东北部经历了250~150 Ma缓慢埋藏增温过程,平均增温速率为0.9℃/Ma;150~120 Ma为快速增温阶段,平均增温速率高达2.1℃/Ma,地层温度达到最高,且均大于130℃。之后不同区段经历差异降温过程:北缘露头区经历了120~65 Ma快速降温,平均冷却速率约1.3℃/Ma;65~10 Ma缓慢降温,平均冷却速率约为0.4℃/Ma。南缘露头区及盆地沉降区则经历了120~30 Ma缓慢降温,平均冷却速率约为0.9℃/Ma;30~10 Ma快速降温,平均冷却速率约为1.5℃/Ma。10 Ma以来,盆地东北部整体抬升冷却,平均冷却速率约6.5℃/Ma。分析结果认为燕山中期构造热事件之最高热增温作用的关键时刻为(120±10)Ma,促成鄂尔多斯盆地东北部主要烃源岩层系的成熟生烃和大规模油气成藏。在后期的差异抬升冷却过程中,北缘露头区在65 Ma±通过了110℃等温面,南缘露头区及盆地的沉降区在30 Ma±通过了110℃等温面,有利于相邻地区原生油气藏的积聚和保存,古近纪晚期(30 Ma)尤其是新近纪晚期近10 Ma以来的强烈构造抬升作用有可能是引发原生油气藏调整—改造和次生成藏的关键因素。     

气候变化对山东降水及极端天气气候事件的影响分析

根据新中国成立以来山东省气温资料进行分析,从温度变化来反映山东气候变暖的趋势;在此基础上根据山东省近60年的水文资料分析气候变化对山东降水及极端天气气候事件的影响。结果表明,60年来山东气候呈变暖趋势,随着气候的变化,山东省年降水量呈减少的趋势,并导致极端天气气候事件出现频率及强度呈增大趋势。     

U-Pb Zircon and Re-Os Molybdenite Geochronology of theW-Mo Mineralized Region of South Qinling,China, andtheir Tectonic Implications

A W-Mo mineralized region is located along the northern margin of the South Qinling tectonic belt of China. WMo mineralization occurs mainly in Cambrian–Ordovician clastic and carbonate rocks, and the ore bodies are structurally controlled by NW–SE-and NNE–SSW-striking faults. Evidence for magmatism in the area is widespread and is dominated by intermediate–felsic intrusives or apophyses, such as the Dongjiangkou, Yanzhiba, Lanbandeng, and Sihaiping granitic bodies. Quartz-vein-type mineralization and fault-controlled skarn-type mineralization dominate the ore systems, with additional enrichment in residual deposits. At present, there are few or insufficient studies on(1) the age of mineralization,(2) the relationship between intermediate–felsic granite and W-Mo mineralization,(3) the source of ore-forming materials,and(4) the metallogenic and tectonic setting of the mineralized area. In this paper, we present geochronology results for numerous intrusive granitic bodies in the South Qinling tectonic belt. U-Pb zircon geochronology of the Lanbandeng monzogranite and Wangjiaping biotite monzogranite yields ages of 222.7 ± 2.3 and 201.9 ± 1.8 Ma, respectively. In contrast to the Late Triassic age of the Lanbandeng monzogranite, the age of the newly discovered Wangjiaping biotite monzogranite places it at the Triassic–Jurassic boundary. Re-Os molybdenite geochronology on the Qipangou W-Mo deposit yielded a model age of 199.7 ± 3.9 Ma, indicating the deposit formed in the early Yanshanian period of the Early Jurassic. Granitoid intrusions in the mineralized area are characterized by composite granite bodies that crystallized at ca.240–190 Ma. While there were multiple stages of intrusion, most occurred at 210–220 Ma, with waning magmatic activity at 200–190 Ma. The Re-Os age of molybdenite in the region is ca. 200–190 Ma, which may represent a newly discovered period of W-Mo metallogenesis that occurred during the final stages of magmatism. The heat associated with this magmatism drove ore formation and might have provided additional ore-forming components for metallogenesis(represented by the Wangjiaping biotite monzogranite). Ore materials in the mineralized area were derived from mixed crustal and mantle sources. Enrichment of the region occurred during intracontinental orogenesis in the late Indosinian–Yanshanian, subsequent to the main Indosinian collision. At this time, the tectonic environment was dominated by extension and strike-slip motion.     

胶东威海地区榴辉岩退变质的地球动力学信息

威海地区榴辉岩退变质过程表现为三个阶段：第一阶段,原生绿辉石分解形成钠质单斜辉石＋斜长石合晶体;第二阶段,原生石榴石及钢质单斜辉石＋斜长石合晶体,周边出现角闪石＋斜长石　状反应边;第三阶段,石榴石及钢质单斜辉石消失。其后榴辉岩相退变质的ｐ－ｔ演化轨迹是压力相对温度快速降低的顺时针形式,反映本区榴辉岩折返的地球动力学过程可能是在经历了快速上升的构造侵位同时,晚元古宙巨量花岗岩浆可将相辉岩块体携带到上部地壳。     

胶辽半岛金伯利岩中地幔捕虏体岩石学特征：古生代岩石圈地幔及其不均一性

华北东部古生代岩石圈地幔经历过复杂的多旋回多阶段熔融岩浆、重结晶、变质和剪切变形历史,因而岩石组成、结构复杂.地幔橄榄岩的主元素、地幔矿物特别是金刚石中的包裹体的Mg#值及Cr#值等显示古生代岩石圈地幔高度难熔亏损玄武质的成分特征,而地幔橄榄岩的不相容元素、同位素显示高度富集的特点.这种高难熔和强富集两重性是克拉通岩石圈地幔的特征.Pb同位素反映华北东部古生代岩石圈地幔具冈瓦纳大陆地幔的特点.复县和蒙阴古生代岩石圈地幔尽管都表现为太古代克拉通地幔的特征,但存在着不均一性,前者受克拉通化后的深部作用影响强于后者.与新生代地幔Sr、Nd同位素对比表明富集的古生代岩石圈地幔向亏损新生代的地幔转变和减薄伴有新生地幔物质对古老岩石圈的置换和混合作用.