云南澜沧地区南角河银多金属矿床的地质特征及成因

南角河银多金属矿是在地质调查过程中发现并评价的一个具有大型找矿远景的矿床。矿床产于临沧-勐海复式花岗岩基南段西侧与新元古界澜沧群变质岩的接触断裂破碎带(白章断裂)中,矿体呈脉状,形态单一。同位素及成矿流体分析结果表明,成矿物质主要来源于花岗岩和澜沧群地层,成矿流体以大气降水下渗加热上升回返并混合少量岩浆热液为特征,以花岗岩和澜沧群变质岩为矿源层,以断裂破碎带为赋存空间,为具有明显垂向分带特征的低温热液矿床。     

滇池磷的现代沉积与环境污染防治对策

在滇池磷现代沉积的实验资料研究,特别是磷块岩生物成矿作用研究的基础上,提出了滇池污染防治的优化对策,即在滇池培养聚磷菌,使其种类及繁衍量大于解磷菌的种类与繁衍量,水体中的磷便可向底泥迁移沉积,底泥中的磷向水体释放也会得到有效控制,富营养化自然改观,环境污染逐渐改善。     

Geochronology and Geochemistry of Mafic Rocks in the Xuhe, Shaanxi, China: Implications for Petrogenesis and Mantle Dynamics

The Xuhe mafic rocks, located in Ziyang county of Shaanxi Province, are dominated by diabase-porphyrite, gabbro–diabase, diabase, and pyroxene diorite. Primitive mantle-normalized multi-element patterns show that, the Xuhe mafic rocks are enriched in large ion lithophile elements(LITE), such as Ba and Pb, depleted in K and Sr for basic rocks, and are depleted in Sr, P and Ti for pyroxene diorite. Chondrite-normalized REE patterns display LREE enrichment(LaN/YbN = 9.34–13.99) and have normalized patterns for trace element and REE similar to that of typical OIB. Detailed SIMS zircon U–Pb dating yields emplacement ages of 438.4 ± 3.1 Ma for Xuhe mafic rocks. The relatively low Mg O(basic rock: 3.11–7.21 wt%; pyroxene diorite: 0.89–1.21 wt%) and Mg#(0.20–0.49) for Xuhe mafic rocks suggest that they were possibly originated from an extremely evolved magma. The rising parental mafic magmas underwent pyroxene and plagioclase fractionation. Crustal contamination of pyroxene diorite before emplacement occurred at a higher crustal level compared to other lithology in Xuhe mafic rocks. The degree of partial melt was low(5%–10%) and in garnetspinel transition facies. Sr-Nd isotope of pyroxene diorite and enrichment mantle characteristics for Xuhe mafic rocks suggest that mafic rocks in the North Daba Mountains were derived from a mixture of HIMU, EMII and small amount of EMI components. Furthermore, this study discusses mantle geodynamic significance of Xuhe mafic rocks in the Silurian, which indicates subduction and uplift of magma caused back-arc extension.     

我国古代记录的特殊流星现象与现代印证

中国古代有着大量的对于流星和流星雨的观测记录，最早可以追溯到3000多年以前。在这些珍贵的记录中，不仅有对于流星的一般描述，而且还有一些至今不能完全理解的特殊流星现象的记录。基于现代对电声变换流星声、流星体的螺旋线形运动、流星的颜色变化和流星的分裂等等的研究，列出在中国古代文献中可以查找到的有关记录。这些记录，不仅是世界文化宝库的一部分，而且对于今天的研究仍有实用价值。对电声变换流星声的报道，只是近20年来，才确立了的并非是观测者的臆想。流星的现代彩色照相观测，更真实地记录和展现了其他的特殊流星现象和它们的发生与演变。这些古代记录与现代的流星观测的对比，可以起到相互印证的作用。     

Observations of EUV and soft X-ray recurring jets in an active region

We present simultaneous observations of three recurring jets in EUV and soft X-ray (SXR), which occurred in an active region on 2007 June 5. By comparing their morphological and kinematic characteristics in these two different wavelengths, we found that EUV and SXR jets had similar locations, directions, sizes and velocities. We also analyzed their spectral properties by using six spectral lines from the EUV Imaging Spectrometer (EIS) onboard Hinode and found that these jets had temperatures from 0.05 to 2....     

Chemical mixing by turbulent convection in the overshooting region below the convective envelope of RGB stars

Based on the turbulent convection model(TCM),we investigate chemical mixing in the bottom overshooting region of the convective envelope of intermediatemass stars,focusing on its influence on the formation and extension of blue loops in the Hertzsprung-Russell(HR) diagram.A diffusive mixing model is adopted during the Red Giant Branch(RGB) phase.The properties of the blue loop are changed by modification of the element profiles above the H-burning shell,which results from the incomplete mixing in the bottom...     

Experimental studies on the evolution process of microcrack patterns in concrete samples con-taining hard inclusions

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在真三轴压缩条件下片麻岩破裂孕育过程中弹性波的特征变化

片麻岩在真三轴压缩至主破裂的孕育过程中，沿σ３方向（与主破裂面斜交）的弹性波有显著的特征变化；Ｐ波、Ｓ波的初至波走时变化呈现略高～平稳～高值～（回降）的形式，走时比呈现平稳～低值～回升的变化特征。振幅呈现低值～平稳高值～下降～（低值）变化形态，振幅比呈现相对稳定～甚高值～回降变化形态。波列振幅衰减系数呈现稳定值～低值～回升变化形态。微裂隙的开闭和Ｐ，Ｓ波的非同步变化及相对变化量的不同是上述特征变化的主要原因     

GPS对滇西北土地覆盖的遥感多波段光谱响应特性分析 --以大中甸乡为例

分析覆盖地物的遥感光谱响应特性对于利用遥感监测土地覆盖是非常必要的。基于GPS实地调查，利用ETM 数据，采用全数字化遥感定量方法对大中甸乡典型土地覆盖地物多波段光谱响应特性进行研究。结果表明，该区13种典型覆盖地物，同属于非植被类型与同属于植被类型覆盖地物所表现的响应特性曲线形态具有明显差异，NDVI表现出以数值0为分界限，大于0为植被地物，小于0为非植被地类；另外，光谱响应分析还应考虑遥感信息获取的时相特性。     

三江并流带环境地质与基础设施建设对策浅析

三江并流带位于印度板块与欧亚板块的缝合线部位，新构造运动强烈，构造发育，岩石破碎，地势陡峻，地质环境异常脆弱，地震、滑坡、崩塌、泥石流等地质灾害频繁。区内旅游资源、生物资源、水利资源、矿产资源、人资源极为丰富，是西部大开发中极有前景的地域，亟需加强基础设施建设。为了保护三江并流带的自然环境、生态环境、地质环境，在公路、水电等基础设施的建设中，应该采取开发与保护并重的对策。本针对该区新构造运动发育、岩石强烈破碎的特点，分析在公路、水电等基础设施建设中给区域环境地质带来的不良影响，并提出处治措施与对策建议。