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341.
井间地震串联滤波波场分离方法 总被引:2,自引:0,他引:2
严又生 《物探化探计算技术》1997,19(3):210-215
本文根据井间地震波场响应以及多种波场分离方法的性能,采用基于K-L变换的特征向量滤波与中值滤波相结合的串联滤波方法分离井间地震观测到的上、下行反射波。数值计算结果表明:在波场分离过程中,由于同时综合考虑了地震波能量主分量分布以及反射波同相轴时差两个参数,使得分离效果明显、处理更为简便,具有滤波特征矢量的选取条件更为宽松、无需精确确定拉平轴的时间等特点。 相似文献
342.
在岩溶地区,地下水的超强度开采与工业“三废”及生活废弃物不合理的排放,造成了地下水较严重的污染。用动态系统方法建立的地下水污染时间序列递推预测模型,在岩溶地下水环境质量预测与管理方面都具有指导意义。 相似文献
343.
相山铀矿田成矿作用的地球化学模拟 总被引:4,自引:0,他引:4
相山铀矿田是我国最大的火山岩型热液铀矿田,在地质地球化学和高温高压实研究的基础上,利用地球化学模式程序EQ3/6模拟了成矿热水溶液的形成过程和减压排泄区铀成矿作用。计算机模拟结果表明,通过大气降水与碎斑熔岩相互作用,可以形成富含F和SiO2等矿化剂的含铀热水溶液;由于铀以UO2F^3和UO2(CO3(^2-3等配合形式存在,非常稳定,即使在深部强还原环境中仍能能够迁移;酸性和碱性环境,尤其是强酸性 相似文献
344.
Chemical composition of upper crust in eastern China 总被引:4,自引:0,他引:4
In an area of 3.3×106 km2 within eastern China, 28 253 rock samples were collected systematically and combined into 2718 composite samples which were
analyzed by 15 reliable methods using national preliminary certified reference materials (CRMs) for data quality monitoring.
The average chemical compositions of the exposed crust, the sedimentary cover and the exposed basement as well as the upper
crust for 76 chemical elements in eastern China are given.
A key basic geology projcct supported by Ministry of Geology and Mineral Resources of China. 相似文献
345.
By contrasting and analyzing the characteristics of gravity field nearby some important active faults in the continent of
China, it can be found that the crust blocks where Bouguer anomalies are regionally positive (or relatively positive) are
moving towards the terrestrial poles and the blocks where Bouguer anomalies in a tremendous area are negative (or relatively
negative) are moving towards the equator. By analysis of mechanics and mathematics calculation and based on lots of practical
data, the authors hold that the change in density of a crust block is a decisive factor that causes the horizontal movement
of the continental crust, while magma activity is an important factor that leads to the change in density of a crust block. 相似文献
346.
Based on characteristics and trap types of gas reservoirs in large and medium gas fields in China, 4 gas reservoir models
have been established:(i) structural trap gas reservoir model I, formed earlier than or simutaneously with generating of gases;
(ii) structural trap gas reservoir model II, formed later than generating of gases; (iii) fossil weathered residuum gas reservoir
model; and (iV) mud diapir abnormal temperature and pressure gas reservoir model. Distribution patterns of large-medium gas
fields are described with the concept of “sealed compartment”. It is concluded that the inner-compartment area, marginal area
of the compartment and the areas between two overlapped sealed compartments are the most favourable areas for discovering
large-medium gas fields.
Project supported by the “85–102” Chinese National Key Science and Technology Project. 相似文献
347.
Evolution model and formation mechanism of bio-thermocatalytic transitional zone gas 总被引:1,自引:0,他引:1
As a new genetic type of natural gas exploration area, the bio-thermocatalytic transitional zone gas (BTTZG) has been highly
stressed by geologists both at home and abroad. Systematic study on the generation mechanism of hydrocarbon at the transitional
zone is presented. Based on simulating experiments and geochemistry analysis of the source rock with lower evolution, a hydrocarbon-forming
model at the transitional zone has been established. The mechanism is proposed that under the condition of low temperature
and pressure combining with extremely active structural stress and clay mineral catalysis, BTTZG is formed by de-group of
soluble organic matter and polarized compositions through orthocarbon ion as well as by condensation polymerization of aromatic
ring-rich insoluble organic matter. This mechanism controls the formation of BTTZG, and furthermore, BTTZG is the product
of superimposition and interaction of all the factors mentioned above. 相似文献
348.
Evolution of Quaternary groundwater system in North China Plain 总被引:4,自引:0,他引:4
Zonghu Zhang Dehong Shi Fuhong Ren Zhengzhou Yin Jichao Sun Cuiyun Zhang 《中国科学D辑(英文版)》1997,40(3):276-283
The Quaternary groundwater system in the North China Plain is formed mainly through the terrestrial water flow action on the
united geological and tectonic backgrounds. The analysis of groundwater dynamic field, simulation of groundwater geochemistry,
and the14C dating and extraction of isotope information have provided more evidence for recognizing and assessing the evolution of
groundwater circulation system and studying the past global changes. The exploitation and utilization of groundwater on a
large scale and overexploitation have given rise to the decline of regional groundwater level, change of flow field, decrease
of water resources and downward movement of saline water body. The water environment has entered a new evolution stage in
which it is intensely disturbed by the mankind’s activities.
Project supported by the National Natural Science Foundation of China. 相似文献
349.
泌阳凹陷核桃园组微量元素演化特征及其古气候意义 总被引:31,自引:6,他引:31
泌阳凹陷下第三系核桃园组总体上表现为一个大的湖退体系,而其中的微量元素含量及有关元素比值却呈现出细微而明显的旋回变化特征。本文依据泥岩、页岩和碳酸盐岩中Ti、Sr、Ba等十六种微量元素含量及Sr/Ba、Fe/Mn、Sr/Cu等七种比值的变化特征,结合古盐度及岩相资料,对核桃园组沉积时的古气候作了系统的研究,基本上分出了温暖潮湿、干湿交替、炎热干旱、温热半干旱四类较为特征的古气候类型,以期为油气勘探提供依据。 相似文献
350.