汞元素的石油地质意义

油气中都含有汞元素组分,汞的物理化学性质决定其可以从油气藏中向上垂向运移,根据采样介质类型及样品预处理的手段不同,地表中汞的分析方法可分为壤气、热释汞及土壤总汞分析方法。壤气汞、热释汞及土壤总汞指标都有着很好的示油气意义,同时也有着示断裂带的地质意义。     

欧北地区深层三维地震采集技术

辽河盆地由于其特殊的地震地质条件,以往采集的深层地震资料信噪比和分辨率都较低,已经严重制约了油田的进一步勘探和开发.为了彻底摆脱地震资料品质对勘探工作的束缚,努力提高资料的信噪比和分辨率,辽河油田首先选择辽河盆地东部凹陷欧利坨子北为突破口,通过采取最佳岩性激发、有效弱信号保护和变观测系统施工等一系列的技术措施,取得了较好的效果.     

The Role of Fracture Structure in Leachate Pollution at Landfills： A Case Study of a Landfill in Chongqing City

This paper studies a landfill where there are three faults running through.As serious pollution has occurred to the geological environment,the landfill is to be closed up and renovated.The paper aims to explore the role of fracture structure in leachate pollution at the landfill.The research was carried out in several stages.First,mathematical models of the pre-renovation landfill with three faults running through and the landfill after renovation were established.And then,the boundary conditions and parameters of the two mathematical models were determined.The groundwater level of the landfills was simulated in order to modify the two mathematical models.As a result,a feasible mathematical model was achieved.Based on this model,a comparison was made of the COD concentration variations in the inside leachate and outside leachate between the two landfills. Accordingly,the impacts of the fracture structure on the pollution of leachate at the landfills could be identified.The study results show that while faults contribute to the migration of leachate,they also serve as a confluence of leachate,thus further deteriorating the environment.The COD concentrations of the inside leachate and the outside leacbate of the pre-renovation landfill are respectively 800 mg/L and 220 mg/L higher than those of the post.renovation landfill.Therefore,measures must be taken to handle the leachate seepage in areas where there are faults as well as the neighboring areas so as to get the environmental pollution under control.     

The Role of Fracture Structure in Leachate Pollution at Landfills: A Case Study of a Landfill in Chongqing City

This paper studies a landfill where there are three faults running through. As serious pollution has occurred to the geological environment, the landfill is to be closed up and renovated. The paper aims to explore the role of fracture structure in leachate pollution at the landfill. The research was carried out in several stages. First, mathematical models of the pre-renovation landfill with three faults running through and the landfill after renovation were established. And then, the boundary conditions and parameters of the two mathematical models were determined. The groundwater level of the landfills was simulated in order to modify the two mathematical models. As a result, a feasible mathematical model was achieved. Based on this model, a comparison was made of the COD concentration variations in the inside leachate and outside leachate between the two landfills. Accordingly, the impacts of the fracture structure on the pollution of leachate at the landfills could be identified. The study results show that while faults contribute to the migration of ieachate, they also serve as a confluence of leachate, thus further deteriorating the environment. The COD concentrations of the inside leachate and the outside leachate of the pre-renovation landfill are respectively 800 mg/L and 220 mg/L higher than those of the post-renovation landfill. Therefore, measures must be taken to handle the ieachate seepage in areas where there are faults as well as the neighboring areas so as to get the environmental pollution under control.     

祁阳山字型构造质疑

结合区域构造演化背景及构造变形特征,对祁阳弧形构造的形成机制进行研究。分析表明,传统山字型构造机制难以解释祁阳弧形构造的诸多特征,且前人认为变形动力来源于东西向挤压应力场,也与印支期区域构造应力场实为NWW向的构造背景不符,因此祁阳弧形构造并不属典型山字型构造。基于研究区构造活动的客观实际,提出祁阳弧形构造的可能形成机制:NW向基底隐伏断裂和NNE-NE向主干断裂分别于印支期和燕山期产生强烈左旋走滑活动,从而使区域NNE向构造线在中段产生左旋偏转成为NNW向,从而形成S形的祁阳弧形构造。这一机制可较好解释祁阳弧形构造的若干特征,如关帝庙穹窿呈NWW走向、北反射弧构造形迹不显著、北弧弧顶脱位及内弧曲率大于外弧、南弧弧顶脱位、紫云-中田-高峰串珠状穹窿的形成等。上述认识对华南地区弧形构造研究具有一定启示意义:除山字型构造作用和砥柱作用外,还应注意断裂走滑等其他构造活动对弧形构造的制约,以及多次构造活动叠加对构造形迹可能造成的影响。     

胶东地区晚中生代岩浆活动及对大地构造的制约

应用近十几年来胶东地区及其周边岩浆岩体的同位素测年资料,结合几个岩体的新的SHRIMP测年数据(牙山岩体117.7Ma,院格庄岩体113.4Ma,正长斑岩脉115.7Ma),系统研究了该区晚中生代以来的岩浆活动规律,结果表明,该区可分为4个岩浆活动期;(1)晚侏罗世构造-岩浆热事件(150~160Ma),以玲珑-滦家河型岩体为代表,是在区域挤压构造应力作用下侵入的,属同构造或同造山时期的岩浆作用。(2)早白垩世早期构造-岩浆热事件(135~125Ma),以郭家岭岩体为典型,该时期的岩浆活动均具有双峰式岩浆作用特征,反映了伸展动力学背景。(3)早白垩世中晚期构造-岩浆热事件(125~105Ma),以崂山花岗岩为特征,该阶段对应于中国东部岩石圈大规模的减薄时期,是大陆裂谷作用的高峰期。(4)晚白垩世-古新世基性-超基性火山作用。本文还探讨了岩浆活动的地球动力学因素及其对大地构造的制约。     

新疆温泉县北达巴特斑岩铜钼矿地质特征及成因初探

北达巴特斑岩铜钼矿产于华力西期流纹斑岩中,矿体呈脉状,铜矿体地表为氧化物,钼矿体主要赋存于深部的流纹斑岩中,其矿化作用呈上铜下钼的双层矿化结构模式,矿化为细脉浸染状。矿床的成因类型为斑岩型铜钼矿。     

基于GPS数据的浑河断裂带抚顺市区段现今活动性定量分析

浑河断裂带是深大断裂-郯庐断裂的北延分支,横贯抚顺市区,在断裂带之上及其两侧建有诸多大型工矿企业及民用建筑,断裂带的稳定与否关系到抚顺市的城市安全。近期,浑河断裂带抚顺市区段的个别次级断裂发生活动,并已造成严重的城市建筑破坏。局部断裂活动的成因,为城市决策者所关注。本文利用抚顺市城市平面控制网相隔17a的两期GPS测量数据,应用大地形变分析的理论方法,对浑河断裂带抚顺市区段的稳定性进行了定量分析,得出结论:浑河断裂带抚顺市区段的宏观地质构造在此期间活动性不明显。     

基于GPS的四川地区现时地壳形变分析

对四川区域网多年数据进行处理,得到欧亚框架下的测站运动速度,采用刚性地块假设下的最小二乘拟合方法,得到川滇、川青、扬子地块的运动速度分别为(17.6±1.0)mm/a、(11.4±0.7)mm/a、(9.6±1.1)mm/a,地块运动方向逐渐由SE向SEE变化;作为川滇地块东边界的鲜水河断裂、安宁河-则木河断裂运动速度远大于龙门山断裂,显示了其较强的活动性。     

对北秦岭太阳寺矿集区金矿成矿特征的初步认识

甘肃省天水冯家场—两当太阳寺一带,是近年来资源评价和矿产勘查的重点,是秦岭-大别成矿省北秦岭成矿带中重要的矿化集中区。文章在分析区域构造背景的基础上,对该区成矿特征进行了初步总结,选择典型矿床进行了介绍,初次把该区命名为太阳寺矿集区,这将对该区矿产勘查工作部署,深入研究矿集区成矿规律具有参考意义。