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101.
本文对Ni40Mn30Fe30合金与在不同焙烧温度下得到的含水叶蜡,在高温超高压下的反应进行了实验研究,温度测至1420℃,压是至5.5GPa,研究了该反应的物质-化学机制,以及反应速率与温度,压力,含水量等参数的关系,对高压下物质迁移运动的固有特征进行了探讨。 相似文献
102.
A Study on Organic Inclusions in Clastic Reservoir Rocks and Their Application to the Assessment of Oil and Gas Accumulations 总被引:5,自引:0,他引:5
Terrigenous clastic reservoir rocks are widespread in China,and nearly all the industrial oil and gas accumulations in eastern China occur in the clastic rocks.The study shows that organic inclusions are mostly distributed in the secondary fissures and pores which were ormed in the process of oil-rock interaction,rather than in the cements or secondary enlargements. The organic inclusions are dominantly organic gas-rich or are composed of pure hydrocarbons.Homogenization temperatures range mainly from 120℃ to 130℃,which shows a relatively high maturity of organic matter.Vertical and horizontal temperature changes provide the grounds for the investigation of basin evolution and thermal fluid-kinetics-model.Fluorescence spectral characteristics o the organic inclusions indicate that oils and gases in the area studied probably have experienced two-stage or two-time migration.Micro-fluorescence rescearch is one of the effective approaches to oil/source correlation and oil migration-stage determination.The abundance and occurrence of organic inclusions is one of the indicators of oil and gas abundance and accumulation in rock layers.With the help of other informatio,organic inclusions can provide the basis for the prospective assessment of oil and gas in clastic reservoir rocks. 相似文献
103.
This paper presents a method of establishing a hydrothermal ore-forming reaction system.On the basis of the study of four typical hydrothermal deposits,the following conclusions concerning geochemical dynamic controlling during hydrothermal mineralization have been sions concerning geochemical dynaamic controlling during hydrothermal mineralization have been drawn:(1)The regional tectonic activities control the concentration and dispersion of elements in the ore-forming process in terms of their effects on the thermodynamic nature and conditions of the ore-forming reaction system.(2)During hydrothermal mineralization the activites of ore-bearing faults can be divideb into two stages:the brittle splitting stage and the brittle-tough tensing stage,which would create characteristically different geodynamic conditions for the geochemical thermodynamic ore-forming system.(3)The hydrothermal ore-forming reaaction system is an open dynamic system.At the brittle splitting stage the system was so strongly supersaturated and unequilibrated as to speed up and enhance the crystallization and differentiation of ore-forming fluids.And at the brittle-tough tensing stage,the ore-forming system was in a weak supersaturated state;with decreasing temperature and pressure the crystallization of oreforming material would show down,and it can be regarded as an equilibrated state.(4)In the lates stages of hydrothermal evolution,gold would be concentrated in the residual ore-forming solution.The pulsating fracture activite in this stage led to the crush of pyrite ore and it was then filled with gold-enriched solution,forming high-grage“fissure”gold ore.This ore-forming process could be called the coupling mechanism of ore formation. 相似文献
104.
水/岩作用实验研究表明,在低温条件下柠檬酸、草酸和酒石酸对岩石中的铁、铜都有很高的淋滤率。这表明,在表生地质作用过程中有机酸对成矿元素有很强的活化能力。实验研究同时发现,有机酸对成矿元素的活化能力受其分解温度的限制,由于大部分有机酸的分解温度都在250℃以下,因而有机酸对成矿元素的活化仅限于低温条件。本次研究还显示,判断一种岩石能否成为矿源层,不能简单的以其中成矿元素的含量高低作为标准,其中更关键的因素是元素在岩石中的存在形式,如果成矿元素在岩石中难以活化的形式存在,那么含量再高也无法提供成矿物质 相似文献
105.
云南腾冲热泉金的有机地球化学研究——Ⅰ生物标志物浅析 总被引:1,自引:1,他引:1
本文主要通过对比分析研究热泉软泥中的金含量与有机质及含硫化合物的相关性。并测定泉水及软泥中含金量和软泥中有机碳含量,以及对抽提物中的饱和烃和芳烃族组分进行色谱—质谱分析,最后得出的结论:有机质的沉积环境为还原—强还原,有机质属于腐泥-腐殖型,接近和达到了成熟阶段。软泥中金含量与有机质的性质无明显相关关系,与有机碳含量也无明显相关关系,而与其成熟度相关密切。样品分析证实软泥中含硫化合物与金含量呈正相关性。对比分析了水及软泥中金含量,认为两者之间也无明显相关关系 相似文献
106.
Sediment-hosted gold deposits are the major type of gold resources in china,Concen trated mostly in the two“Triangle Regios“,they are generally hosted in fine-clastic turbidite,hydrothermal chet and marl ranging from cambrian to Triassic in age,structurally controlled by domes,anticlines and second-ordered faults.They are similar to the Carlin-type gold deposits in mineral assemblage and geochemical marks,with an element association closely comparable to those of modern springs and submarine hydrothermal sediments.Organic matter may have played an important role in mineralization .The ore solution may be hydrothermally altered meteoric water developed i areas of local geothermal anomaly. 相似文献
107.
广州珠江西航道,流溪河有机污染特征与感潮作用 总被引:6,自引:3,他引:6
珠江西航道和流溪河在广州市区上游,为广州市主要水源区。由于感潮作用,受市区严重污染的水体因涨潮上溯而上游传输。严重影响上游水质。因此,弄清感潮作用对广州水源区水质的影响程度和范围,对水源保护与利用有重要意义。本研究从下游到上游,对水源区底泥中有机物特征进行了分析,结果表明:(1)从上游到上游,受感潮作用影响逐渐减小,污染程度逐渐减轻;(2)水源区有机物特征呈有规律变化。从靠近城市的下游到远离城市的 相似文献
108.
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
109.
The hydrocarbon generation mechanism and the three-stage type model of hydrocarbon generation for carbonate source rocks 总被引:1,自引:0,他引:1
The diagenetic mechanism and process of carbonate rocks, which is different to that of clastic rocks, decides the existence
of different existing state organic matters in carbonate rocks. This has been verified by both the microscopic observation
of organic petrology and the analysis of organic geochemistry of many samples. Based on the hydrous pyrolysis simulation experiment
of the low-mature carbonate rocks, the contrasting study on the yield and their geochemistry characteristics of different
existing state soluble organic matters of a series of various maturity samples shows that the different existing state organic
matters make different contributions to hydrocarbon generation during every evolution state. So that, the hydrocarbon generation
process of carbonate rocks can be summarized as the following three stages: the first is the direct degradation of biogenic
bitumen macromolecules during the immature stage, the second is the thermal degradation of a large amount of kerogen at the
mature stage, the last stage is the expulsion or release of inclusion organic matter owing to the increased thermal expansion
pressure during the high evolution stage.
Part of achievements of the Eighth Five-Year National Science-Technology Key-Task Project “85-102-02-07”. 相似文献
110.
Organism relics or kerogens in oils are first obsenred by a confocal laser scanning microscope (CLSM) and a transmission electron
microscope (TEM). The complexes of kerogens in oils are characterized by the presence of a great variety of microfossils or
macerals. These kerogens in oils are mainly the residues of the original organic substances from which oil formed, and minor
kerogens from enclosing rocks enter the oils, therefore, the components and types of the kerogens in crude oils can serve
as an indirect indicator of oil-source rock correlation. This method was applied to Jurassic oils in the Junggar Basin and
the Turpan-Hami Basin, and there are two types of the kerogens in oils: one containing a lot of macerals from terrestrial
plants may derive from coals, and the other, characterized by a high content of microscopic algae, fungus spores and Acritarch,
may originate from Permian organic matter. In addition, the reflectance of the vitrodetrinites in oils can be used as an indicator
of oil-source rock correlation. 相似文献