共查询到20条相似文献，搜索用时 78 毫秒
1.
应用阶段加热技术 ,对中国东部新生代玄武岩中的橄榄岩包体和大别造山带超高压榴辉岩进行了包裹体 CO2 的碳同位素组成测定。结果表明 ,橄榄岩的δ1 3C值变化较大 ,从 - 2 2 .8‰到 0 .7‰ ,明显不同于前人报道的低δ1 3C值 (- 2 8‰～- 2 0‰ )特征 ,指示中国东部地幔流体中 CO2 的碳同位素组成是不均一的 ,反映了地壳有机碳与原生地幔碳的混合特征。大别造山带榴辉岩的 δ1 3C变化从 - 18.5‰到 4 .6‰ ,同样明显不同于前人报道的低 δ1 3C值 (- 30‰～ - 2 0‰ )特征。榴辉岩的低δ1 3C值指示了板块俯冲前其玄武岩原岩受到地表含有机碳流体蚀变后的碳同位素特点 ,而较高的δ1 3C值反映了板块折返过程中榴辉岩受淋滤大理岩的富 CO2 流体叠加的退变质效应。橄榄岩包体和超高压榴辉岩的轻碳同位素共同特点反映了板块俯冲引起的壳—幔物质相互作用和碳同位素地球化学再循环 ,指示中国东部岩石圈地幔含有丰富的地壳有机碳组分 相似文献
2.
加拿大阿尔伯达省西部上泥盆统凯恩组白云岩的成因 总被引：1，自引：0，他引：1
加拿大阿尔伯达省西部上泥盆统凯恩组主要由粉晶白云岩和细晶白云岩组成，另外还常见一种充填溶蚀孔洞的亮晶白云石。粉晶白云岩纹理、泥裂和鸟眼等构造发育，其δ＾１３Ｃ为＋１．０‰－＋３．０‰，δ＾１８Ｏ为－６．０‰－－４．３‰，为潮坪上混合水白云化形成。细晶白云岩分布于假整合面之下，其δ＾１３Ｃ为＋０．２‰－＋２．９‰，δ＾１８Ｏ为－６．９‰－－４．６‰，也是混合水白云化的产物。亮晶白云石洁净明亮、晶粒粗 相似文献
3.
王台山地区韧性剪切带型金矿成因 总被引：1，自引：0，他引：1
五台山地区韧性剪切带型金矿分布地晚太古代碰撞造山带中，与世界许多太古宙绿岩带型金矿具有相似的特征。研究表明：成矿流体的δ＾１８ＯＨ２Ｏ＝－２．１‰－４．９‰，δＤ＝－６９－１１２‰，蚀谜面对得起盐矿物的δ＾１３ＣＰＤＢ＝－２．０－１．４‰，δ＾１８ＯＳＭＯＷ－１０．０－２０．０‰，载金黄铁矿的δ＾１４Ｓ＝－３．７－５．６‰。成矿前流体具有一高盐度，成矿期流体以富含ＣＯ２、近似海水的δ＾１８Ｏ和海相 相似文献
4.
扬子地台震旦纪海水碳同位素的变化 总被引：15，自引：1，他引：15
本文测定了湖北宜昌三峡剖面震旦系海相碳酸盐岩样品的碳同位素组成。研究表明：震旦纪扬子区海水的δ＾１３Ｃ值显示出大幅度变化，南沱冰期δ＾１３Ｃ为低值（－４‰）；陡山沱早期δ＾１３Ｃ值迅速上升，达到５－６‰，陡山沱期δ＾１３Ｃ值一般在０－５‰之间；灯影期δ＾１３Ｃ值较平稳，一般在２．０－３．４％之间，导致震旦经水δ＾１３Ｃ值大幅度变化的原因主要是由于以疑在和近岸为藻类等光合作用的海洋植物群体为主体的大 相似文献
5.
大别－胶南造山带温泉气中的ＣＯ２含量较低（多数在１．００％以上）,δ＾１３Ｃ变化范围为－２０．３４‰至－３．０‰,主要为源于地壳浅层的有机成因气。整个造山带各温泉气体成分均以Ｎ２为主（９０％左右）,其来源除大气Ｎ２以外,可能为地壳岩石释放或地层中有机体演休形成。稀有气体同位素组成表明,Ａｒ主要来源于大气,Ｈｅ为壳内岩石放射成因。本区温泉气体地球化学特征可能与现今中国东部的构造应力场有关,即大别－胶 相似文献
6.
结合碳酸盐岩层序地层分析，首次系统测定了马平组碳，氧同位素值，并对其演化规律与层序地层的关系进行了探讨，研究结果表明：马平组内δ＾１３Ｃ，δ＾１８Ｏ值变化范围分别是－２．５６‰～＋３．８９‰和－８．１６‰～－６．０２‰（ＰＤＢ）准层序为δ＾１３Ｃ值向上逐渐减小，海进体系域（ＴＳＴ）和高水位体系域（ＨＳＴ）内δ＾１３Ｃ值分别呈增加和减小的趋，层序界面处δ＾１３Ｃ，δ＾１８Ｏ值均表现为负异常，控制层序 相似文献
7.
深源流体—老王寨金矿床含矿流体来源的一种可能性 总被引：6，自引：1，他引：6
老王寨金矿床含矿流体是一种富含矿化剂Ｃｌ＾－、ＣＯ２和Ｓ＾２－的高温高压深源流体。石英中流体包裹体的δ＾１８ＯＨ２Ｏ值在＋６．９１‰￣＋１１．７６‰之间，δＤＨ２Ｏ值为－６８．１０‰￣－１０１．１０‰之间，辉锑矿的δ＾３４Ｓ值为－０．１５‰￣－１．０３‰，方解石的δ＾１３Ｃ值为－０．３４‰￣－３．１２‰。研究结果表明，这种流体既不是岩浆热液也不是大气降水，而是一种深源流体。 相似文献
8.
苏北东海榴辉岩氢氧同位素地球化学研究 总被引：14，自引：0，他引：14
研究了苏鲁地体西部东海地区超高压变质榴辉岩的氢氧同位素组成,得到绿辉石和石榴子石的δ＾１８Ｏ值变化较大（为－１０．４‰－＋４．８‰）,多硅白云母的δＤ值变化较小（为－１０４‰－－８３‰）不同矿物对之间达到保存了氧同位素平衡,得到了一致的同位素温度（６５０－７５０℃）,榴辉岩具有低至－１０‰和－１０４‰的异常δ＾１８Ｏ和δＤ值表明,岩石与极贫＾１８Ｏ和Ｄ的大气降水成因流体发生过氢氧同位素交换,同时排 相似文献
9.
天然气碳同位素部分反序与乙烷碳同位素特征的模拟研究 总被引：4，自引：1，他引：3
通过煤系源岩热模拟烃类气地球化学研究,结合源岩自然演化形成天色气的研究,认为煤原岩在热演经进行中,随化程度增高δ＾１３Ｃ１值从轻变重,δ＾１３Ｃ２变化较小,在低演化阶段一般为－２８‰±（Ｒｏ＝０．４５％～０．５６％）,当源岩进入生烃门限阶段δ＾１３Ｃ２值一般为－２６‰～２３‰左右。且随热演化程度增高进一步变重,但一般不大于－２０‰。烃类气碳同位素系列４ 部分反序现象,不仅仅是不同成因天然气混源特征 相似文献
10.
云南兰坪三山—白身坪铜银多金属成矿富集区的碳氧同位素地球化学 总被引：9，自引：0，他引：9
研究区的碳氧同位素组成表明,矿化灰岩和细晶灰岩的δ＾１３Ｃ为正值,其δ＾１８Ｏ值变化于－６．４‰～－２１‰之间;而绝大多数矿石中碳酸盐矿物的δ＾１３Ｃ为负值,只有少数为正值,与其对应的δ＾１８Ｏ值为－１２．３‰～－１２．５‰。根据δ＾１３Ｃ－δ＾１８Ｏ图解分析,区分出了３种不同类型的碳同位素：（１）三叠纪海洋生物碳;（２）海相碳酸盐的碳与热卤水中碳的过渡类型;（３）深部热卤水中ＣＯ２的碳。研究发现 相似文献
11.
《International Geology Review》2012,54(6):665-675
In the U. S. S. R., so far, none of the hydrocarbon pools at depths exceeding 3500 m have been exploited. There are reasons to believe that large accumulations exist even below 5000 m depths, in areas shown on the map (fig. 1). Almost nine-tenths of proved economic reserves of oil and gas at shallow depths lie in terrigenous materials, the remainder in carbonates, in fissure-type-collectors. It is believed that the latter type of collectors will be found to be more abundant at greater depths. -- V. P. Sokoloff 相似文献
12.
Alessandro Beghini Zdeněk P. Bažant R. Chambon D. Kolymbas I. Herle 《国际地质力学数值与分析法杂志》2004,28(4):365-372
13.
V.V. Vladimirov 《Geoforum》1984,15(1):19-23
Regional planning in the U.S.S.R. is part of a comprehensive and hierarchical spatial and sectoral planning system. Four levels are described: (a) the national level, involving the total settlement system; (b) the major regional level, handling major development schemes; (c) the minor regional level, with plans for administrative districts; and (d) the urban level, where city master plans are produced. The amount of detail and scale of working increased downwards through the hierarchy. The most pressing problem is planning for the emergence and growth of cities of 100,000 population or more. Moscow city-region is used as an illustration. 相似文献
14.
《International Geology Review》2012,54(1):23-26
On October 12, 1962, a joint session of the Presidium of the U.S.S.R. Academy of Sciences and the Collegium of the U.S.S.R. Ministry of Geology and Mineral Reserves adopted a resolution “On the present state of the geological sciences in the U.S.S.R. Academy of Sciences and the U. S. S. R. Ministry of Geology and Mineral Reserves and their prospects for the future.” Important contributions of Russian geologists are acknowledged, but attention is drawn to many shortcomings. Future goals of geological study and work are given in detail. Twenty-one lines of research to be concentrated on are given, covering all phases of geology, geophysics, and geochemistry. In discussing the failings of the geological profession in Russia, it is of interest to note the following comment: “Geological research in other countries is still insufficiently studied and applied, and we are not making adequate use of geologic information from abroad.” The list of the Russian geologists' shortcomings sounds vaguely familiar. —J. R. Hayes 相似文献
15.
The morphology of paleosols and radiocarbon-dated charcoal from buried surface horizons of soils provide evidence to suggest that between periods of northward forest encroachment tundra climate has dominated areas at least 50 km south of the present forest/tundra border in southwest Keewatin. The present forest/tundra border climate is nearly as severe as any climate that has prevailed in the area since deglaciation. 相似文献
16.
17.
The thermal stabilities and decay kinetics of three peroxy radicals (Centers #1, B and B′) and three other radiation-induced
defects (#3, C′ and E1′) in natural quartz from the high-grade McArthur River uranium deposit (Athabasca basin, Canada) have been investigated by
isochronal and isothermal annealing experiments and electron paramagnetic resonance (EPR) spectroscopy. Single-crystal EPR
spectra of isochronally (2 h) annealed quartz show that these centers all grow in intensity to 280°C and then decay with further
increase in temperature, but their disappearance temperatures differ markedly and depend on the initial concentrations (e.g.,
Center #1 in a dark smoky quartz is annealed out at 380°C, B and B′ at 420°C and #3 and C′ at 580°C). The isothermal decay
processes of these centers are all of the second order type. The calculated activation energies for the peroxy radicals [#1
and B + B′ at 0.36 (9) and 0.83 (8) eV, respectively] are smaller than those of Centers #3, C′ and E1′ [1.09 (8), 1.24 (8) and 1.45 (7) eV, respectively]. Gamma-ray irradiations of thermally bleached quartz restore a fraction
of the peroxy radicals, suggesting that their diamagnetic precursors are stable up to at least 800°C. The unusual decay characteristics
of “peroxy radicals” in quartz reported in the literature are shown to most likely arise from multiple radiation-induced defects.
These results have implications for not only applications of peroxy radicals in quartz for EPR dating but also better understanding
of thermoluminescence and cathodoluminescence spectra of this mineral. 相似文献
18.
19.
20.
Kenneth PALMER Paul C. KENNEDY Barry ROSER 《Geostandards and Geoanalytical Research》1983,7(2):301-303
The concentrations of 20 trace elements in 6 British Chemical Standards (BCS) reference materials and 5 European Federation of Refractories Producers (PRE) reference materials have been determined by X-ray fluorescence spectrometry. 相似文献