加卸载响应比理论在中强地震（7〉M≥6）预测中的应用

本文运用加卸载响应比理论对中强地震前的加卸载响应比的变化进行了研究。结果表明，中强地震前加卸载响应比明显上升，表现为三种不同的形态，持续时间为半年到两年。     

湖北峡东地区灯影组石板滩段微化石

本文研究了发现于湖北峡东地区，震旦系灯影组石板滩段燧石夹层岩石薄片中的微古植物化石，包括１０属５种（其中１新属新种）和５个未定种，石板滩段黑色薄层灰岩以富含宏观藻类及碳质印膜和少量后生动物而闻名，我们在燧石夹层牟岩石薄片中，不仅发现上述宏观藻类，而且首次发现共生的微化石。及其他保存很好的微化石，这一发现进一步丰富 我国震旦纪的古生物资料，为地层对比提供了依据。     

频率测深波区视电阻率响应和正演计算

本文对频率测深电偶源发射时的波区视电阻率响应进行了较系统的讨论,指出了国内现有理论中的一些错误。研究发现,在进行波区视电阻率响应的理论推导时,当基底电阻率有限时进行零级近似是正确的,但当基底电阻率为无限大时,进行零级近似是不完善的,必须进行修改。利用正确的公式进行了视电阻率响应的正演计算,结果表明,利用零级近似得出的公式与利用一级近似得出的公式计算的视电阻率响应曲线首支部分符合较好,但对于有高阻基底存在的地电断面,响应曲线尾支差异很大。     

云南临沧地区帮卖盆地含铀煤中锗矿的研究

帮卖盆地是一个不对称山间向斜盆地,其基底为海西·燕山期(γ~3_4-γ~2_5)花岗岩体。盖层为新第三纪的含煤碎屑岩。锗矿体大部分存在于N_1~2煤层中。含铀煤主要为变质程度低的褐煤,属于半暗-半亮煤、暗亮煤及亮暗煤。锗在煤中的存在形式:1.主要为腐植酸锗络合物及锗的有机化合物;2.一部分呈吸附状态;3.极少数呈类质同象。     

动态聚类-模糊模式识别及其应用

本文以模糊子集论为指导,在迪戴的DCM法的基础上提出了动态聚类-模糊模式识别方法。实际上,它是一种新的模糊聚类的方法。该方法以DCM法的动态聚类部分做为原始数据变换的手段,而将迪戴的强模式概念推广为模糊模式,将强模式识别推广为模糊模式识别。此外,还提出了模糊模式间联系度的概念,从而解决了类间联系、类内典型个体、类间过渡个体、个体对各类的隶属程度以及内部有某种演化趋势的类别的划分等问题。文章还给出了该方法的数学模型和算法概要。最后,通过一个在地质学中的应用实例,说明了该方法的应用效果。     

Morphological responses of<Emphasis Type="Italic">Limnocythere inopinata</Emphasis> (Ostracoda) to hydrochemical environment factors

Living ostracod and hydrochemical samples were collected synchronously from more than 50 lakes and small water body in the eastern edge area of the Tibetan Plateau, Northern Tibetan, Southern Tibet and mid-Tibet. The comparison of the adult body length ofLimnocythere inopinata and hydrochemical parameters of their habitats shows that a quantitative relationship exists between the adult body length and salinity expressed as conductivity. An empirical formula to reconstruct paleosalinity is suggested first and applied to salinity reconstruction of CE-2 core from Cuoe Lake, Tibet. The method is verified by comparing its outcome with results of other environment reconstruction methods.     

广州白云山常绿阔叶林的结构特征

在线路调查和样方调查的基础上分析了广州白云山常绿阔叶林的结构特征.群落主要由亚热带科属组成,优势科为芸香科、五加科、茜草科、山茶科、壳斗科、鼠刺科、樟科等.优势树种也以相应的优势科属树种为主.群落中胸径≥3cm的个体密度较小,只有1964株/hm2;群落较为低矮,平均高度只有6m;乔木垂直分化不明显,树种水平分布不均.白云山的植被是次生植被和人工造林改造的结果,只在山谷少数植被没受人类干扰.其现状植被是天然次生植被和人工植被的混合体.在一些由马尾松发展起来的群落,天然侵入的阔叶树种已在主要层中居优势;群落中可见马尾松衰退的痕迹.     

对GPS接收机测试评估的探讨

随着GPS的广泛应用和GPS产业的迅速发展，GPS厂家众多，生产的接收机类型更是数以百计，整个GPS接收机市场可以说是鱼目混珠，识别困难；大多数购买者只能听信厂家的技术指标，如何对GPS接收机的性能进行测试评估的意义显得很重要，本文基于此对GPS接收机测试评估展开探讨和研究。     

Least-squares self-coherency analysis of superconducting gravimeter records in search for the Slichter triplet

We develop a new approach for the spectral analysis of the superconducting gravimeter data to search for the spheroidal oscillation ₁S₁ of the Earth solid inner core. The new method, which we call least-squares (LS) self-coherency analysis, is based on the product of the least-squares spectra of segments of the time series under consideration. The statistical foundation of this method is presented in the new least-squares product spectrum theorem that establishes rigorously confidence levels for detecting significant peaks. We apply this approach along with a number of other innovative ideas to a 6-year long gravity series collected at the Canadian Superconducting Gravimeter Installation (CSGI) in Cantley, Canada, by splitting it into 72 statistically independent monthly records. Each monthly record is analysed spectrally and all monthly LS spectra are multiplied to construct the self-coherency spectrum of the 6-year gravity series. The self-coherency spectrum is then used to detect significant peaks in the band 3-7 h at various significant levels with the aim to identify a triplet of periods associated with the rotational/ellipsoidal splitting of ₁S₁ (Slichter triplet). From all the Slichter periods predicted by various researchers so far, Smylie's triplet appears to be the most supported one, albeit very weakly, both, before and after the atmospheric pressure effect is removed from the series. Using the viscous splitting law [Smylie, D.E., 1992. The inner core translational triplet and the density near Earth's center. Science 255, 1678-1682] as guide, we can also see one interesting and statistically significant triplet with periods A = {4.261 h, 4.516 h, 4.872 h}, which changes slightly to A′ = {4.269 h, 4.516 h, 4.889 h} after the atmospheric pressure correction is applied to the gravity series.