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941.
临沧超大型锗矿床有机质与锗矿化的地球化学特征 总被引:10,自引:3,他引:10
临沧锗矿床是一产于第三系含煤岩系中的超大型矿床。矿床的最初锗源与盆地西缘的二云母花岗岩有关。主矿体产于下煤组沉积旋回的早期地层中,每一沉积阶段早期形成的褐煤和碳质泥岩中富含锗,最高含量达1470×10^-6。褐煤和碳质泥岩在矿化过程中平均富集了164-169倍。根据锗含量,褐煤和碳质泥岩可分为锗含量小于12×10^-6的低锗煤(泥岩)和大于90×10^-6的高锗煤(泥岩)。高锗煤中有机质富含氧官能 相似文献
942.
Taking the active fault network as the structural frame, the Chinese mainland and its periphery can be regarded as a system of "fault movement and seismogeny." By using the self-coupling method, preliminary study shows that the seismogenic system is a time-ordered dissipation system. The time order in the state far from equilibrium is established and maintained through mass and energy exchanges between the system and the surroundings. The evolution of the seismogenic system follows some properties of unbalanced phase change, namely, critical retard, bifurcation, entropy reduction, etc. 相似文献
943.
Zhou Cuiying Wang Hongwei Wang Mei and Zhang YuxiaSeismological Bureau of Shandong Province Jinan China Center for Analysis Prediction SSB Beijing China 《中国地震研究》1997,(4)
In order to solve the problem of early estimation of moderately strong aftershock duration time in an earthquake sequence,this study has been conducted.First,the definition of the strong aftershock has been given.It is pointed out that there is a difference in the strong aftershock duration time between the main shock type sequence and the strong earthquake swarm sequence.After dividing the three cases,i.e.,a strong aftershock duration time larger than 1 day,smaller than 1 day,and no strong aftershock occurred in a main shock type sequence by using the pattern recognition method,we gave the rough correlation relation between strong aftershock duration time and first large shock magnitude for two types of sequences.Finally,the judgment index and method of estimating strong aftershock duration times for different sequence types have been given. 相似文献
944.
Dong Ruishu Xiang Hongfa Guo Shunmin Ran Hongliu and Fu ChanghongInstitute of Geology SSB Beijing China Institute of Geophysics SSB Beijing China 《中国地震研究》1997,(4)
There have been 12 possible locations of the earthquakes occurring in the South Yellow Sea since 1505.In this paper,the location of the earthquake that occurred in 1505 has been determined by the collection of more historical data of the influenced field,referring the isoseismal data of earthquakes with the epicentral intensityⅨ and combining geophysical field data with tectonic condition,due to its great influence on seismic safety assessment of some significant engineering. 相似文献
945.
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
946.
Magnetostratigraphy and palaeoclimate of Red Clay sequences from Chinese Loess Plateau 总被引:5,自引:0,他引:5
Two Red Clay profiles near Xi’an and Xifeng were investigated in an attempt to determine magnetostratigraphic and palaeoclimatic
records. The results show that aeolian dust accumulation and the related East Asia palaeomonsoon system had begun by 6.5 Ma,
and it is deduced that the Tibetan Plateau had reached a significant elevation at that time. The late Tertiary palaeoclimatic
history of the Red Clay as reflected by magnetic susceptibility is reconstructed during the period of 6.5–2.5 Ma. Stepwise
increase in susceptibility of aeolian dust accumulation appears to have a close correlation to the uplift processes of the
Tibetan Plateau. The remarkable increase of aeolian dust accumulation at 3.2 Ma appears to be due to the influence of global
ice volume on the East Asia monsoon. Palaeomonsoon variation during the late Tertiary as recorded in the Red Clay sequences
from the Chinese Loess Plateau can be regarded as the product of a number of interacting factors, such as uplift of the Tibetan
Plateau, solar radiation, global ice volume, etc.
Project supported by the National Natural Science Foundation of China and the Foundation of Xi’an Laboratory of Loess and
Quaternary Geology, Chinese Academy of Sciences. 相似文献
947.
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
948.
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
949.
线性度方法在前兆观测数据分析处理中的应用 总被引:3,自引:1,他引:3
利用空间线性度方法,对前兆场中不同台站,不同学科的前兆观测数据从总体形态上进行综合分析,得到关于描述前兆场的新的特征量a(空间线性度)本文给出了空间线性度的具体计算方法,并以华北地区为例,分析处理了区内1970~1994年部分地电阻率和地下水位观测资料,所得结果表明,新的前兆特征量a在中强地震之前一年左右时间内有异常显示。 相似文献
950.
近年来的一些研究表明,由于地震前孕震区地下介质的电性结构的变化,将导致地磁短周期转换函数发生异常变化。通过对地震前后的地磁短周期转换函数的参数的计算、分析和研究,有可能提取出可靠的地震短临前兆异常(曾小苹等,1990)。为了进一步开展对该方法研究工作并使其在我区地震预测预报研究中得到应用,我们使用了静海台的地磁记录资料,分析计算了该台地磁短周期转换函数在地震前后的变化情况,确立了该方法应用天津地区地震预报的短临异常特征及指标,取得了较好的效果。 相似文献