阿拉善地区找矿新进展——珠斯楞海尔罕铜多金属矿

1∶20万区域化探扫面发现的AS26号综合异常,经1∶5万水系加密测量和三级查证,找到了异常源,发现了珠斯楞海尔罕Cu、Au矿。综合物化探普查,在此矿带内圈出2km2高视极化率、低视电阻率激电异常和低缓磁异常。已施工的槽、井工程和ZK9801孔均见矿。沿走向,激电异常和磁异常在东、西两端均未封闭,有大幅度向外延伸趋势,可能是深部硫化物矿层向外延伸的反映。     

黄河下游河床纵向与横向变形的数值模拟——Ⅱ二维混合模型的应用

对前文提出的平面二维混合模型进行了验证与实际工程应用.模拟了概化顺直河段在不同冲淤条件下的河岸后退过程.将混合模型应用于实际工程问题,模拟了黄河下游花园口游荡型河段的河床纵向与横向变形过程.通过对断面平均水位、流速分布、断面形态变化等计算值与原型观测值的对比,两者符合较好.表明该混合模型不仅能较好地模拟出河道内的水沙运动与河床纵向冲淤过程,而且能模拟出滩岸的后退与淤长过程,尤其能模拟滩岸的冲刷与崩塌过程.     

Titanian clinohumite–garnet–pyroxene rock from the Su-Lu UHP metamorphic terrane, China: chemical evolution and tectonic implications

A garnet–pyroxene rock containing abundant Ti-clinohumite (ca. 40 vol.%) occurs along with eclogites as small blocks in quartzo-feldsparthic gneiss in the southern end of the Chinese Su-Lu ultrahigh-pressure (UHP) metamorphic terrane. It consists of three aggregates: (1) Ti-clinohumite-dominated aggregate with interstitial garnet and pyroxene, (2) garnet+pyroxene aggregate with Ti-clinohumite inclusions, and (3) Ti-clinohumite-free aggregate dominated by garnet. Apatite, phlogopite, zircon, hematite, pentlandite, and an unknown Ni-Fe-volatile-Si (NFVS) mineral, which is replaced by Ni-greenalite, occur as accessories. Serpentine is the major secondary mineral. Garnet (Prp_63.9–64.6Alm_25.8–26.9Grs_1.4–7.9Uva_0.5–7.6Sps_1.0) in all three aggregates is pyrope-rich with very low grossular component, with that in the aggregate (2) most enriched in Cr (Cr₂O₃=2.55 wt.%). Orthopyroxene is depleted in Al (Al₂O₃=0.16 wt.% in the cores) and Ca (CaO=0.06–0.09 wt.% in the cores), with X_Mg (Mg/(Mg+Fe)) values at ca. 0.900. Clinopyroxene is chromian diopside with Fe³⁺≥Fe²⁺. Matrix clinopyroxene has a lower X_Mg (0.862) than that (0.887) included in Ti-clinohumite. The rock contains modest amount of heavy rare earth elements (HREE) (10 to 12×C1 chondrite), with significant enrichment in Cr, Co, Ni, V, Sr, and light rare earth elements (LREE) (22 to 33×C1 chondrite). The clinopyroxene is very enriched in Cr (Cr₂O₃ is up to 2.09 wt.% in the cores) and Sr (ca. 350 ppm) and LREE (Ce_N/Yb_N=157.7). Ti-clinohumite is enriched in Ni (1981 ppm), Co (123 ppm), and Nb (85 ppm).

While it is possible to enrich ultramafites in incompatible elements in a subducted slab, the high Al, Fe, Ti, and low Si, Ca, and Na contents in the Ti-clinohumite rock are difficult to account for by crustal metasomatism of an ultramafite. On the other hand, the similarity in major and trace element compositions and their systematic variations between the Ti-clinohumite-garnet-pyroxene rock of this study and those of Mg-metasomatised Fe–Ti gabbros reported in the literature suggest that crustal metasomatism occurred in a gabbroic protolith, which resulted in addition of Cr, Co, Ni, and Mg and removal of Si, Ca, Na, Al, and Fe. This implies that the rock was in contact with an ultramafite at low pressure. During subsequent subduction, the metagabbro was thrust into the country gneiss, where gneiss-derived hydrous fluids caused enrichment of Sr and LREE in recrystallised clinopyroxene. P–T estimates for the high-pressure assemblage are ca. 4.2 GPa and ca. 760 °C, compatible with those for the eclogites and gneisses in this terrane. It is possible that the Ti-clinohumite-garnet-pyroxene rock and associated eclogites represent remnants of former oceanic crust that was subducted to a great depth.     

Late Paleozoic faults of the Altai region, Central Asia: tectonic pattern and model of formation

The present kinematic and dynamic analysis of large-scale strike-slip faults, which enabled the formation of a collage of Altai terranes as a result of two collisional events. The Late Devonian–Early Carboniferous collision of the Gondwana-derived Altai-Mongolian terrane and the Siberian continent resulted in the formation of the Charysh–Terekta system of dextral strike-slip faults and later the Kurai and Kuznetsk–Teletsk–Bashkauss sinistral strike-slip faults. The Late Carboniferous–Permian collision of the Siberian and Kazakhstan continents resulted in the formation of the Chara, Irtysh and North-East sinistral strike-slip zones. The age of deformation of both collisional events becomes younger toward the inner areas of the Siberian continent. In the same direction the amount of displacement of strike-slip faulting decreases from several thousand to several hundred kilometers. The width of the Late Paleozoic zone of deformation reaches 1500 km. These events deformed the accretion-collision continental margins and their primary paleogeographic pattern.     

水泥土搅拌桩复合地基载荷试验数值分析

水泥土搅拌桩在高速公路的软基处理中得到了广泛应用,但是对水泥土搅拌桩地基深层桩土应力比和变形未能有深入的认识.笔者应用弹性层状体系和Mindlin附加应力联合求解的方法,对水泥土搅拌桩复合地基载荷试验进行数值分析计算,总结了水泥土搅拌桩复合地基深层桩土应力比的变化规律,讨论了水泥土搅拌桩复合地基深层桩土变形协调问题.     

基于Bayes原理的复合地基承载力概率分析方法

从Bayes的基本原理出发 ,研究了复合地基承载力的概率分析方法。结合实测数据 ,推导了承载力后验分布统计量的计算公式 ,对复合地基承载力的先验公布进行了修正     

CFG桩复合地基问题

对CFG桩复合地基设计、施工和检测问题进行了探讨,提出了CFG桩复合地基亟待研究的问题.     

土工格栅加筋垫层用于处理特殊地基

某地两幢拟建于软土地基上的建筑物,原设计均采用PHC管桩基础。在桩基施工过程中分别发现软基中有大量孤石和条石(古码头遗址),桩基无法施工。经多方论证,最后采用水泥搅拌桩复合地基配合土工格栅加筋垫层的处理方案。其中一幢建筑已竣工,经现场荷载试验和沉降观测检验,地基承载力和沉降完全满足工程要求,且降低了造价。     

路堤荷载下CFG桩复合地基沉降分析

分析了路堤荷载下CFG桩复合地基的变形机理，根据假定的沉降模式及桩侧摩阻力分布形式，推导出了考虑桩-土-褥垫层共同作用的简化沉降计算公式，结果与试验数据吻合较好。     

Formulating a General Spatial Segregation Measure*

Most traditional segregation measures, such as the index of dissimilarity D, fail to distinguish spatial patterns effectively. Previously proposed spatial measures modifying D suffer from several shortcomings. This article describes a general spatial segregation index based upon the concept of composite population counts, which are derived from grouping people in neighboring areas together to account implicitly for spatial interaction of groups across unit boundaries. The suggested spatial index can overcome the disadvantages of previous indices and can assess the spatial extent of the segregated clusters. The results offer a more comprehensive depiction of spatial segregation of a region.