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81.
马家沟灰岩(古)岩溶研究中的若干问题探讨 总被引:4,自引:0,他引:4
讨论了华北地区奥陶系马家沟组灰岩岩溶研究中的几个问题,包括沉积岩溶,暴露岩溶,埋藏岩溶,现代岩溶及陷落柱等,指出了沉积岩溶和暴露岩溶洞穴不能保存或保存甚少,但对后期的岩溶发育具有重要控制作用,最后,提出了今后奥陶系灰岩岩溶研究的基本思路。 相似文献
82.
南方海相油气勘探为什么久攻不下? 总被引:7,自引:0,他引:7
中国南方从震旦纪到三叠纪8个地质时代海相地层厚度巨大,具有很大的生烃能力。然而除四川地区之外,至今油气勘探尚无重大突破。积十二年对南方5个地质时代海相地层基础地质研究及制图的经验,认为南方海相油气勘探久攻不下的原因是:(1)对整个南方还缺乏全面的、历史的,整体的和深刻的认识;(2)还不于用什么方法或顺序去认识它。建议重视基础地质研究,并以中国南方二叠纪及三叠纪的岩相古地理研究和制图为例,提出基础地 相似文献
83.
利用高分辨率卫星影像进行地震损失评价所需的城市特征识别 总被引:2,自引:0,他引:2
高分辨率卫星影像已经在一些国家的民用领域得到应用。利用高分辨率卫星影像来收集地震损失评价所需要的各类城市信息不仅高效和有较好的时间分辨率,而且它可以减少以往所必需的大量的代价高昂且费力的城市调查。基于在印度城市台拉登所做的研究,讨论了如何利用高分辨率卫星影像进行城市特征识别的一些问题,同时也简单论述了利用GIS/RS软件综合所得的数据以便用于地震损失评价的方法。 相似文献
84.
地热井井位确定研究——以豫煤二队院内地热井为例 总被引:2,自引:0,他引:2
通过对龙门地热田地质构造、地下水运动特点及规律的研究,提出了在地热田内寻找地下热水的富水靶区,并推算了其范围。又以地面调查、地面电法等手段进行了验证,确定了地下热水富水带的具体位置及地热井施工井位,一次成功地打中千米以下地热水的富水区,为地热田内寻找、开发地下热水总结了经验,丰富了深井及地热田找水的理论。 相似文献
85.
根 据 开 滦 集 团 赵 各 庄 矿 业 公 司 水 文 地 质 情 况 和 居 民 用 水 的 现 状 ,提 出 全 天 供 水 的 新 观 念 ,即 将 全 年 需 集 中强 排 的 水量 变 为 人 们日 常 生 活 的用 水 量 ,既 解 决 了 分 时 间 段 供 水 给 职 工 生 活 造 成 的 不 便 ,提 高 了 人 们 的 生 活 质 量 ,又 合理 的 利用 了水 资 源,而且 还可 以 降低 奥灰 水 对安 全生 产 的威 胁。 相似文献
86.
利用激光粒度仪测试超细煤粉的粒度。对测试超细煤粉试样粒度时的试样浓度、测试温度、分散时间、分散剂的种类及浓度等方面的影响进行了实验研究,给出了激光粒度仪测试超细煤粉粒度的最佳实验条件。 相似文献
87.
Several theoretical, empirical and semi-empirical methods are available in the literature to predict settlement of drilled
shafts in sandy soils. In the Arabian Gulf countries, specifically in the United Arab Emirates, equations and procedure from
the rest of the world are being used in analysis and design of drilled shafts without proper validation. It is the aim of
this study to assess the applicability and evaluate the accuracy of two well known, and commonly used methods for pile prediction
in the United Arab Emirates (UAE), namely Vesic (1977) and Poulos (1979), via comparison with data from field pile load tests
conducted on shafts drilled in the region. Some of these tests were conducted for the purpose of this study, while others
were made available through the courtesy of International Piling Contractors who are active in the region (e.g. Bauer International
and Swiss Borings). Pile load test data were analyzed to back-calculate the model parameters related to settlement under different
loading stages. Geological data and soil properties were obtained from studies conducted at the relevant sites. An effort
is made to correlate soil properties with the prediction models. Statistical analysis is conducted to assess the accuracy
of the results obtained from the two methods at different stages of loading via those obtained from pile load tests. Moreover,
a detailed parametric study is conducted to assess the effect of the related parameters on the predicted pile settlement and
the estimated settlement at different stages of loading. The study concluded with a recommendation of the most appropriate
models and procedures to be followed for predicting the settlement of drilled shafts in the UAE, together with useful charts
and correlation relations. Results showed that settlement values predicted by Vesic (1977) and Poulos (1979) overestimates
the true values.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
88.
The Significance of Multiple Saturation Points in the Context of Polybaric Near-fractional Melting 总被引:1,自引:0,他引:1
Experimental petrologists have successfully located basalticliquid compositions parental to mid-ocean ridge basalt thatare, within experimental resolution, multiply saturated withthree-phase harzburgite or four-phase lherzolite assemblageson their liquidus at some elevated pressure. Such an experimentalresult is a necessary consequence of any paradigm in which eruptedbasalts derive from single-batch primary liquids that equilibratewith a mantle residue and undergo no subsequent magma mixingbefore differentiation and eruption. Here we investigate whether,conversely, such evidence of multiple saturation is sufficientto exclude dynamic melting models wherein increments of meltare mixed after segregation from residues, during melt transportor in magma chambers. Using two independent models of crystalliquidequilibria to simulate polybaric near-fractional peridotitemelting, we find that aggregate liquids from such melting processescan display near-intersections of liquidus surfaces too closeto distinguish experimentally from exact multiple saturationpoints. Given uncertainties in glass compositions, fractionationcorrections, experimental temperature and pressure conditions,and achievement of equilibrium, these results suggest that polybaricmixtures can in fact masquerade as mantle-equilibrated single-batchprimary liquids. Multiple saturation points on the liquidussurfaces of primitive basalts do, however, preserve informationabout the average pressure of extraction of their constituentincrements of liquid. KEY WORDS: mantle melting; basaltic volcanism; experimental igneous petrology; thermodynamic modelling; inverse method 相似文献
89.
NEKVASIL H.; DONDOLINI A.; HORN J.; FILIBERTO J.; LONG H.; LINDSLEY D. H. 《Journal of Petrology》2004,45(4):693-721
Experimental simulation of incremental crystal fractionationof a hy-normative hawaiite indicates that the spectrum of compositionsfrom mildly alkalic hawaiite to sodic rhyolite found in silica-saturatedalkalic suites of the ocean islands and continental hotspotsand rifts can be produced by fractionation at 9·3 kbarwith bulk water contents > 相似文献
90.
KADIK A.; PINEAU F.; LITVIN Y.; JENDRZEJEWSKI N.; MARTINEZ I.; JAVOY M. 《Journal of Petrology》2004,45(7):1297-1310
Studies of iron-bearing silicate melt (ferrobasalt) + iron metallicphase + graphite + hydrogen equilibria show that carbon andhydrogen solubilities in melts are important for the evolutionof the upper mantle. In a series of experiments conducted at3·7 GPa and 15201600°C, we have characterizedthe nature (oxidized vs reduced) and quantified the abundancesof C- and H-compounds dissolved in iron-bearing silicate melts.Experiments were carried out in an anvil-with-hole apparatuspermitting the achievement of equal chemical potentials of H2in the inner Pt capsule and outer furnace assembly. The fO2for silicate meltiron equilibrium was 2·32 ±0·04 log units below ironwüstite (IW). Theferrobasalt used as starting material experienced a reductionof its iron oxides and silicate network. The counterpart wasa liberation of oxygen reacting with the hydrogen entering thecapsule. The amount of H2O dissolved in the glasses was measuredby ion microprobe and by step-heating and was found to be between1 and 2 wt %. The dissolved carbon content was found to be 1600ppm C by step-heating. The speciation of C and H componentswas determined by IR and Raman spectroscopy. It was establishedthat the main part of the liberated oxygen was used to formOH and to a much lesser extent H2O, and only traces ofH2, CO2 and 相似文献