东秦岭石界河群中石榴石成分环带所记录的PTt轨迹     

李荣西  胡能高  安三元  杨家喜 《地球科学与环境学报》1993,(Z1)

位于河南省西峡县北部地区的石界河群榴云片岩中的石榴石发育有很好的结构和成分环带。本文应用微分热力学方法对其环带成分进行计算,确定出一条顺时针方向的PTt轨迹。该轨迹与应用矿物共生组合世代关系确定的PTt轨迹十分吻合。  相似文献   

城市综合功能GIS开发问题研究     

龚强  胡运权 《地理信息世界》2001,(1)

首次提出了城市综合功能地理信息系统并对其作了介绍 ,在此基础上 ,对应用模式、开发问题、开发注意事项等进行了讨论。  相似文献   

潼峪金矿区成矿断裂构造特征     

钱壮志  胡正国 《地球科学与环境学报》1992,(3)

潼峪金矿区发育过冲剪滑型、平移剪张型和平移剪滑型三种不同性质、不同方向成矿断裂,分布在金罗斑背形的不同部位,其形成有先后差异,但变形环境大体相同,具脆-韧性变形特征。空间上一般不超越褶皱主体。三类断裂中,前两者具石英脉型金矿化,后者形成构造蚀变岩型及小规模石英脉型金矿化。矿化差异与断裂产出的褶皱部位及其相应的应力应变条件的不同有关。  相似文献   

一类ENSO事件与四川地区粮食产量的相关分析     

肖天贵  胡毅  谌芸 《成都信息工程学院学报》1992,(4)

本文对1949年以来出现的10次ENSO事件进行了分析,得出如下结果:开始於东太平洋增暖和中大平洋增暖的两类ENSO现象分别对应四川地区粮食产量的减产和增产。此结果对四川地区粮食生产政策的制定及产量的预测研究均有较重要的参考价值。  相似文献   

Two Different Dust Storms in Northeast China:the Sources and Influences in East Asia     

Ke Hu  Yuying Liu  Zhen Cao 《世界地质(英文版)》2003,6(1)

There are two different dust storms in Northeast China, normal dust and alkali dust, from Kerqin sand land and Songnen saline land. As well as visible damages of the dust storms, there are some invisible influences. The authors provide evidences that the bacteria carried by dusts from remote area should not be ignored, but the damages of the alkali dusts are still not clear.  相似文献   

腾冲火山区地表垂直形变分析   总被引：11，自引：3，他引：8  

胡亚轩  施行觉  王庆良  张永志  赵慈平  施发奇  邵德晟 《大地测量与地球动力学》2003,23(2):37-41

对腾冲火山区1998～2000年的3期垂直形变资料进行了分析，进而利用相关资料得出与计算有关的参数，再用多元Mogi模型反演了岩浆房的位置和大小，所得出的结果与地震层析反演结果基本相似。分析反演结果，认为火山区可能存在多个岩浆房，并有岩脉相通。  相似文献   

贺兰山群变质杂岩中的变余动力变质岩     

胡能高  杨家喜  王涛 《地球科学与环境学报》1993,(4)

贺兰山群变质杂岩形成于晚太古代,遭受过多期变质和变形的改造,其中发育了不同期次和层次的动力变质岩。变余韧性剪切带内发育了条带状片麻岩和变粒岩,相伴有变余鞘褶皱和构造透镜体,变余韧性剪切带的变形发生在较低的温度、压力条件下,地壳加厚作用的初期。变余糜棱岩貌似条带状片麻岩,但在青石中保留了早期石英拔丝构造和加粗的动态重结晶长石集合体。糜棱岩化作用的温度在550℃以上,变形后沿面理形成了饼状或椭圆状青石,变晶时温度近600℃,压力近300MPa。  相似文献   

中国强震迁移与现代地壳波浪运动     

胡连英 《地球科学与环境学报》1988,(3)

本文论述了中国强震迁移与现代地壳波浪运动间的关系,指出了中国强震时空分布上的波浪性、方向性及丛集性特征,并将中国强震运动划分为天平式运动、单波系波浪运动、双波系波浪运动、多波系波浪运动等类型,进而对强震机制进行了探讨,指出强震波带和强震丛集区仍是今后强震活动的主要场所。  相似文献   

Oxygen isotope fractionation factors involving cassiterite (SnO₂): I. calculation of reduced partition function ratios from heat capacity and X-ray resonant studies     

V.B. Polyakov  S.D. Mineev  G. Hu  D.A. Khramov  V.E. Gorbunov 《Geochimica et cosmochimica acta》2005,69(5):1287-1300

Oxygen isotope equilibrium fractionation constants (β¹⁸O-factors) of cassiterite were evaluated on the basis of heat capacity and X-ray resonant (Mössbauer spectroscopy and X-ray inelastic scattering) data.The low-temperature heat capacity of cassiterite was measured in the range from 13 to 340 K using an adiabatic calorimeter. Results of measurements of two samples agree very closely but deviate more than 5% from previous heat capacity data used for calculation of thermodynamic functions. The temperature dependence of heat capacity was treated using the modern version of the Thirring expansion, and the appropriate temperature dependence of the vibrational kinetic energy was found.Measurements of temperature-dependent Mössbauer parameters of cassiterite were conducted in the range from 300 to 900 K. The attempt to describe Mössbauer fraction and the second order Doppler (SOD) shift on the basis of the Debye model failed. The first term of the Thirring expansion of the Mössbauer SOD shift agrees with that calculated from the Sn sublattice vibration density of states (VDOS) obtained via synchrotron X-ray scattering. Based on this agreement we calculated the kinetic energy of the cassiterite Sn sublattice from VDOS.From the kinetic energy of the total cassiterite crystalline lattice and its Sn sublattice, β¹⁸O-factors of cassiterite were computed in the temperature range 300-1500 K by the method of Polyakov and Mineev (2000). Appropriate polynomials, which are valid at temperatures above 400 K, are the following: