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991.
作者在野外工作中,于遂昌─大柘变质岩断块(下称遂昌变质岩断块)北西侧,麻车─后山垵等地的地表或探矿巷道内,相继发现了多处糜棱岩化岩石露头,认为这一带存在一条较大的韧性剪切带。经对该带的地质,地球化学及金银矿分布的特征的综合分析研究,指出该韧性剪切带有关的金银矿化活动可分为两个期次,即早期金在韧性剪切活动中初始富集,晚期的脆性变形在局部地段形成金矿体。提出在该韧性剪切带找矿工作中,应重视继承韧性剪切带的脆性断裂和断裂带内的浅色蚀变组合及矿化特征。 相似文献
992.
青岛小珠山花岗岩体为中生代偏碱性侵入岩,过去通称小珠山岩体,通过15万区域地质填图,将其划分为15个单元,划归为大店和崂山两个超单元.对各单元的岩石学、岩石化学、微量元素及稀土元素特征等进行了分析研究,认为应属A型花岗岩,为燕山晚期之产物. 相似文献
993.
In arid‐region wadis, groundwater storage lies within shallow Quaternary alluvium deposits, which are connected with the present‐day hydrological cycle and, therefore, are replenished due to occasional runoff and flash flood occurrences. The groundwater resources are precious in these environments; therefore, their potentiality must be assessed with care in the best manner. The aquifer potentiality is calculated after the storativity and transmissivity parameter estimations, which require rather long‐duration field tests with restrictive assumptions in the theoretical model developments, such as the homogeneity and isotropy. It is the main purpose of this paper to expose the fundamentals of the slope‐matching procedure (SMP) and its application for short‐duration field tests in arid‐region aquifers. In this manner, the subsurface hydrogeological behaviours of the bored land pieces at and around the well locations are prospected in a detailed and refined manner. It is shown that in many cases the classical techniques are appropriate, inconvenient and inapplicable with conclusive reliable results and conclusions. The application of the SMP is presented for some aquifer tests from the central western part of the Kingdom of Saudi Arabia. Copyright © 2007 John Wiley & Sons, Ltd. 相似文献
994.
Rainfall weakens an earth slope and triggers mass movement. Relevant triggering mechanisms are complex and include reduction of capillary pressure due to increased saturation and frictional drag on the sediment induced by fluid flow. Physics‐based continuum models utilizing modern computational tools are useful for understanding the mechanisms of deformation in partially saturated slopes; however, they do not provide a scalar indicator called ‘factor of safety’ that measures the potential of a given slope for mass movement. In the present work, we employ sequential calculations consisting of a physics‐based finite element model that couples solid deformation with fluid flow to quantify the stress and deformation fields in a steep hillside slope subjected to rainfall infiltration. This is followed by a limit‐equilibrium calculation based on the method of slices that evaluates the desired factor of safety. The field condition investigated is similar to the steep experimental catchment CB1 near Coos Bay, Oregon, which failed as a large debris flow from heavy rainfall. Copyright © 2011 John Wiley & Sons, Ltd. 相似文献
995.
This paper proposes a numerical model for jointed rock masses within the 3‐D numerical manifold method (NMM) framework equipped with a customized contact algorithm. The strength of rock sample containing a few sets of discontinuities is first investigated. The results of models with simple geometries are compared with the available analytical solutions to verify the developed computer code, whereas models with complex geometries are simulated to better understand the fundamental behavior and failure mechanism of jointed rock mass. Furthermore, the stability of jointed rock mass in an underground excavation is studied, where rock failure process is determined by the 3‐D NMM simulation. The simulation results provide valuable guidance on excavation process design and stabilization design in rock engineering practice. Copyright © 2012 John Wiley & Sons, Ltd. 相似文献
996.
北秦岭存在A、B、C三类火山岩系列,对应着幔源型、壳幔混染型和壳幔混合型成因类型。火山岩系列和成因类型的系统变化,反映了多旋回壳幔物质迁移特证。 相似文献
997.
Two-phase flow in fractured rock is an important phenomenon for a range of practical problems, not the least of which is
non-aqueous phase liquid (NAPL) contamination of groundwater. Although multiphase systems have long been studied in the petroleum
field, in the hydrogeological field progress has only just reaches the point where models are being developed. Scale effect
is one of the main issues of concern. Although models presented in this paper have the potential to provide useful predictions,
they can only be used to investigate a variety of possible scenarios with parameters being specified in the form of distribution
of values. The calibration and validation of all but the simplest of these models poses a formidable task, with great demands
on hydrogeologists and geophysicists to provide adequate data.
Received: 20 May 1996 · Accepted: 19 August 1996 相似文献
998.
姜修道 《地球科学与环境学报》1995,(2)
驾鹿金矿床是小秦岭金矿带中一个比较特殊的矿床类型,产于古老韧性剪切带中,围岩蚀变强烈而广泛,尤其是成脉前的钾长石化。蚀变带及其中的石英脉控制了金矿体的产出,矿床属蚀变岩型金矿,成矿时代为燕山晚期.本文在论述矿床地质特征的基础上,通过稳定同位素研究,认为燕山期构造热事件是成矿的主导控制因素,成矿溶液来自大气降水,成矿物质则部分来自太华群,部分来自上覆中元古界高山河组,矿床成因属大气降水热液矿床. 相似文献
999.
1000.
在坡麓地带进行工程勘察时,应注意论证工程建设对工程地质环境的改变,评价其对设计、施工的适宜性和可行性,采取相应的工程技术措施。 相似文献