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121.
本文通过对秦巴陕、甘、川、豫、鄂五省已知砂金矿床资料的整理和综合,简要的总结了区内砂金矿床的成因,形态类型,不同类型砂金矿床的地质特征及砂金矿的富集规律。对砂金矿的普查找矿工作有一定的指导意义。 相似文献
122.
The favourable synoptic situation and climate background for a sandstorm process,which occurred in theperiod 9—16 April 1988,have been studied through analyzing weather maps,meteorological elements,satellitecloud pictures and sandstorm trajectories.The sand dust origin area,the directions and the paths of sanddust transport,and the extent the sand dust reached are also investigated.The results of measurments andanalysis indicate that the concentration of sand dust particles is 10 times greater than the normal.It is also shownthat the elements in the sand dust are lithophylic and come from natural source through the chemical composi-tion analysis of the sand dust,so that the sand dust has not been polluted by human activities. 相似文献
123.
COMPARISON OF AEROSOL CHARACTERISTICS OVER MAINLAND OF CHINA AND WESTERN PACIFIC AND ITS LONG-RANGE TRANSPORT
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Wen Yupu Yang Shaojin Yang Yinan Chen Bingru Zhou Mingyu Zheng Yueming Zhang Ziyu Yu Hongjian 《Acta Meteorologica Sinica》1991,5(2):160-170
Based on the aerosol data obtained at Shangdianzi regional background monitoring station together withthe air trajectory analysis,the chemical constituents of the aerosol from the different sources are discussed andcompared with the aerosol samples collected over the western Pacific.The results show that the relative massconcentrations of the crustal and pollutant elements in the aerosol collected over the ocean are higher than thosebeing observed at Shangdianzi in particle size above 4.7 μm and below 0.65μm in diameter.The variationsof the enrichment factors of these elements in marine aerosol with particle size are different from those in shang-dianzi's samples.The former enrichment factors are evidently higher than the latter above 1.1 μm in diameter.On the basis of the comparative research,the long-range transport processes of aerosol particles are discussed. 相似文献
124.
四川威远气田烃流体包裹体的研究 总被引:3,自引:0,他引:3
通过烃流体包裹体的类型、均一化温度、气相及液相成分、盐度以及同位素的研究,可以认为威远气田的天然气主要是由白云岩中有机质形成。由于从80~160℃到200~240℃的热解作用,有机物质已演化到过成热阶段。这一过程可由白云岩中存在液态烃及含沥青烃流体包裹体得到证明。威远气田的特征是:震旦系白云岩中天然气的自产自储,以CH_4为主;油田水为古海水,盐度(4.3~17.2)wt%NaCl,pH>8,(CO+CH_4)/CO_2比值指示还原条件。在基底花岗岩石英中发现有气态烃包裹体,其成分及δ~(13)C‰与花岗岩储气层中产出的天然气一致,为部分天然气可能来自深部地壳或地幔提供了新的证据。因而,威远气田天然气的成因主要由有机物质形成,部分甲烷气可能经基底断裂来自地球深处。 相似文献
125.
Data from the super-deep wells(PS10,PS14 and YS1)led to the discovery of widespread met-al-bearing hydrothermal fluids (or hot brines) related to basic magmas in the Lower Tertiary clastic sequence in the Dongpu Depression .In terms of SEM and EDAX analyses, pore-casting thin section examination of sandstone ,the composition and forming temperature of fluid inclusions ,the trace ele-ment composition of mustone and kerogen and organic geochemical analyses, it is demonstrated that the hydrothermal fluids existing in the area studied are ejecting fluids, which have a close bearing on diagenesis and sedimentation, rather than intrusive veins along the tectonic fractures.The main indicators of hydrothermal activity are:(1)abnormal alteration of kerogen;(2) high-temperature altered mineral assemblage;(30abnormal distribution of hydrocarbons;(4) specific assemblages and abnormal contents of heavy metals in mudstone and kerogen;(5) specific composi-tion of complex compounds and assemblages of fluid inclusions in sandstone;(6) periodic basaltic magma activity.Results of geological observations and laboratory simulating experiments demonstrated that the hydrothermal fluids have a close bearing on hydrocarbon generation in the Dongpu Depression. Two aspects of the effect of hydrothermal fluids are noticed:hydrothermal hydrocarbon production and strong metal catalysis in oil and gas generation. 相似文献
126.
海洋可以被分成若干特征各异的、运动着的海水团,各种海洋现象就源于海水团的运动和相互作用。分隔不同海水团的前锋面上的混合作用是促使成矿组分发生沉淀富集的地球化学障。在海水团前锋混合带上,成矿组分在沉积物中产生同生富集,结果生成沉积矿床或矿源层。这是一种在时间上广泛发生但又尚未被人们所认识的崭新机制。 相似文献
127.
浙江杭嘉湖平原区土壤中营养元素丰缺状况的评价 总被引:5,自引:2,他引:5
根据杭嘉湖平原区区域地球化学调查的结果,对本区土壤中农作物营养元素含量及有效量特征进行了评价研究。研究结果表明,本区土壤中营养元素除Mo、S含量表现缺乏外,其它元素为足量和丰富水平。不同土壤中营养元素有效量水平存在明显差异。在区域分布规律上,营养元素的含量及有效量随成土母质、成土过程和人类耕作等因素的不同而显示其差异特征。评价研究结果为本区农业生产中的合理区划、科学施肥、合理种植、土壤改良等提供了重要的地球化学依据。 相似文献
128.
An infrared routine has been developed to estimate the aliphatic portion of kerogen carbon in sedimentary rocks. The procedure does not require isolation of the organic matter and is based on a computer-assisted determination of global band areas in the region of the aliphatic carbon-hydrogen stretching vibrations around 2900cm−1. From these integrated absorptions the amount of aliphatic carbon Cal (mg of aliphatic carbon per gram of solvent-extracted rock) is calculated by means of a calibration with model rocks. Carbonate overtones which interfere in the case of limestones are eliminated by comparison to a CaCO3 standard.The method has been applied to rocks containing kerogens of different types and maturities at TOC levels of 0.5 to 12%. The aliphatic carbon concentrations range from 0.5 to 60mg·g−1 and correlate reasonably well with the residual genetic potentials of the rocks as measured by S2 values from Rock-Eval pyrolysis. The ratio S2/Cal is found to decrease with burial depth reflecting a maturity enhanced conversion of aliphatic carbon to fixed aromatic carbon under Rock-Eval conditions. 相似文献
129.
130.