面块切片在三维地震资料解释中的应用   总被引：1，自引：0，他引：1  

蔡军  龚幸林 《中国煤田地质》2004,16(2):40-41

目前的三维地震资料解释方法仍停留在二维解释的基础上。面块切片解释改变了传统的解释方法，利用了更多的三维信息，比较充分地发挥了三维数据体的三维立体优势，使解释过程更直观、更清楚，提高了解释精度和速度。  相似文献   

煤电钻技术在探放老空水中的应用     

才向军 《中国煤田地质》2004,16(Z1):48-49

通过 对采 空区 积 水规 律的 分 析与 研究 ,提 出在 积 水采 空区 下 沿空 掘进 采 用煤 电钻 探 放水 技术 及 方法 ,解 决了钻 机探 放 水的 塌孔 问 题,既保 证了 沿 空掘 进的 安 全,又 取 得了 较大 的 经济 效益 。  相似文献   

山西墨镫-左权铁路南段地质灾害危险性模糊综合预测评价   总被引：2，自引：0，他引：2  

汪玉松  朱才宝  周爱国  李亚伟 《陕西地质》2004,22(2):84-88

新建铁路工程用地地质灾害危险性评估的特点往往是地质灾害的种类多，影响因素复杂，常规方法不易客观定量的体现各区段在危险性方面的差异。本文在介绍模糊综合评价法基础上，结合实例探讨了模糊综合评价法在新建铁路工程用地地质灾害危险性评价中的应用。  相似文献   

城市桥梁地震碰撞反应研究与发展   总被引：8，自引：5，他引：8  

李忠献  岳福青 《地震工程与工程振动》2005,25(4):91-98

地震时城市桥梁会因邻跨之间的碰撞而发生灾害.本文从桥梁碰撞的模拟模型、发生条件、影响因素、碰撞对桥梁抗震性能的影响以及防止碰撞的措施等方面,对国内外有关城市桥梁碰撞地震反应研究的成果进行了系统的总结和分析,得出以下结论：桥梁碰撞是多因素共同作用所导致的,并使得桥梁的地震反应更加复杂、呈现非线性;要准确评价桥梁地震碰撞反应需要建立更精确的模拟模型;选择合理的邻跨间距和支座宽度以及安装合适的消能减震装置,可有效地减小桥梁的地震碰撞反应.  相似文献   

Geology of the summit limestone of Mount Qomolangma (Everest) and cooling history of the Yellow Band under the Qomolangma detachment     

Harutaka  Sakai  Minoru  Sawada  Yutaka  Takigami  Yuji  Orihashi  Tohru  Danhara  Hideki  Iwano  Yoshihiro  Kuwahara  Qi  Dong  Huawei  Cai  Jianguo  Li 《Island Arc》2005,14(4):297-310

Abstract   Newly discovered peloidal limestone from the summit of Mount Qomolangma (Mount Everest) contains skeletal fragments of trilobites, ostracods and crinoids. They are small pebble-sized debris interbedded in micritic bedded limestone of the Qomolangma Formation, and are interpreted to have been derived from a bank margin and redeposited in peri-platform environments. An exposure of the Qomolangma detachment at the base of the first step (8520 m), on the northern slope of Mount Qomolangma was also found. Non-metamorphosed, strongly fractured Ordovician limestone is separated from underlying metamorphosed Yellow Band by a sharp fault with a breccia zone. The ⁴⁰Ar–³⁹Ar ages of muscovite from the Yellow Band show two-phase metamorphic events of approximately 33.3 and 24.5 Ma. The older age represents the peak of a Barrovian-type Eo-Himalayan metamorphic event and the younger age records a decompressional high-temperature Neo-Himalayan metamorphic event. A muscovite whole-rock ⁸⁷Rb–⁸⁶Sr isochron of the Yellow Band yielded 40.06 ± 0.81 Ma, which suggests a Pre-Himalayan metamorphism, probably caused by tectonic stacking of the Tibetan Tethys sediments in the leading margin of the Indian subcontinent. Zircon and apatite grains, separated from the Yellow Band, gave pooled fission-track ages of 14.4 ± 0.9 and 14.4 ± 1.4 Ma, respectively. These new chronologic data indicate rapid cooling of the hanging wall of the Qomolangma detachment from approximately 350°C to 130°C during a short period (15.5–14.4 Ma).  相似文献   

Cenozoic volcanism and lithospheric tectonic evolution in Qiangtang area, northern Qinghai-Tibet Plateau   总被引：7，自引：1，他引：7  

CHI Xiaoguo  LI Cai & JIN Wei College of Earth Sciences  Jilin University  Changchun  China 《中国科学D辑(英文版)》2005,48(7)

Accompanying with the shortening,thickening and uplifting of the lithosphere,a series of Cenozoic potassic volcanic rock zones are developed in the northern Qinghai-Tibet Plateau.From south to north,the volcanic rocks can be divided into three volcanicrock belts:Qiangtang-Nangqian volcanic belt,Middle Kunlun-Hoh Xil volcanic belt and Western Kunlun-Eastern Kunlun volcanic belt[1].Spatiotemporal evolu-tion of the volcanism and the origins of magmas con-strains on the pulsing uplifting and …  相似文献   

藏北双湖地区上三叠统肖茶卡群的重新厘定及其地质意义   总被引：1，自引：5，他引：1  

冯心涛  朱同兴  李才  林仕良  张启跃  张惠华  曾庆荣  李宗亮 《地质通报》2005,24(12):1135-1140

在双湖地区肖茶卡一带上三叠统肖茶卡群中发现2套砾岩，根据岩石组合、生物化石和界面特征，以2套砾岩为标志层。将原肖茶卡群分解为3个组级岩石地层单位，由下至上分别为肖切堡组、角木茶卡组和日干配错组。从岩石地层、生物地层和层序地层方面阐述了3个组级地层单位的特征和划分的意义。  相似文献   

Dynamic process analyses of saline intrusion with over-exploitation by coupled flow and dispersive modelling     

Fengshan Ma  Y. S. Yang  Z. Cai  M. Chen  R. Yuan 《Environmental Geology》2005,48(6):818-828

Understanding of saline intrusion into coastal aquifer is an important issue in management and protection of groundwater resource, which can be well achieved by groundwater modelling. To explain some phenomena of correlation between groundwater level and salinity in observation wells in coastal area, the authors compare the migration velocity of saline particles and transmission velocity of water pressure and derive analytical equations of these two velocities for plane and radial flows. The driving force and resistance of saline intrusion were analysed based on the analytical modelling. The destruction and reconstruction of the equilibrium between fresh water seepage towards sea and saline dispersion to inland were considered as an essence of whole intrusion process. The dynamic process of seepage and dispersion at different stages of saline intrusion were analysed under groundwater over-exploitation. The basic equations of saline intrusion were derived and the mechanism of transitional zone movement was discussed. These constitute coupled seepage–dispersion theory of saline intrusion, which becomes an important supplement to existing theory of saline intrusion. As a case study on saline intrusion in Guangrao County in Eastern China, this theory was applied to predict the development of saline intrusion in the study area.  相似文献   

地应力与巷道布置关系的理论研究   总被引：4，自引：0，他引：4  

张延新  蔡美峰  欧阳振华 《岩土工程技术》2005,19(2):93-97

初始地应力是地下工程围岩稳定与支护结构设计的一个基本参数。介绍了地应力计算原理 ,并根据矿井实测地应力资料 ,分析了初始地应力场与巷道布置及巷道破坏形式的关系。为今后选择巷道掘进方向和改进巷道支护方案提供了依据。  相似文献   

层状粘弹性介质中SH波的反射、透射问题   总被引：1，自引：0，他引：1  

郭智奇  刘财  张凤琴 《吉林大学学报(地球科学版)》2005,(Z1)

处理粘弹性介质有两种方法,一种是在运动方程中加入介质的粘滞性因素,另一种是从本构方程入手,建立介质的粘弹性模型。后一种方法在研究介质物理性质上具有直接性,是目前使用较为普遍的处理方法。从本构方程的角度,以波尔兹曼(Bo ltzm ann)叠加原理为基础,建立积分型本构方程,进而建立粘弹性介质波动方程,得到二维粘弹性平面波解,并研究了层状粘弹性介质分界面处平面波的反射、透射问题,计算反射、透射系数CR、CT,同时进行了一定的理论分析。  相似文献