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It is shown that the mechanism of directly releasing mantle gas from the magma chambers by taking the faults as the paths controls mantle-derived CO2 reservoir formation,gas source supplement and the geochemical characteristics of the gas,providing further evidence for the mantle genesis of the CO2 reservoirs at the same time.

这表明,幔源气体以断裂为通道自岩浆房中直接释放的机制对于含油气盆地中幔源CO2气藏的形成、气源的补给和气体地球化学特征的塑造起着控制作用,同时也为CO2气藏的幔源成因提供了进一步的证据。

The outgas types and amount of different gas resource varied with the different geological conditions and evolution processes. There are four outgas models including the model in which inorganic gas directly overflows from mantle matter through lithospheric fracture,the model of heat flow piercement outgas,the model of volcano-magma outgas,and the model of carbonate rock outgas due to heat metamorphism.

对气藏成藏条件和深部壳幔结构的研究表明,松辽盆地存在多种类型无机&气源&,由于赋存的地质条件和演化过程不同,不同气源脱气的方式、脱出气体的类型、脱气量也大不相同,共有4种主要的模式:地幔物质沿超岩石圈断裂直接脱气模式;热流底辟体脱气模式;火山—岩浆成因模式;碳酸盐岩热变质成因模式。

Through the channel way of the connnection of the base of Xujiaweizi linked system of faults with partial chamber,the carbonate dioxide gas in the mantle\|derived heat flow diapris move up into appropriate volcanic rock encirclement along the faults, and form gas pool.

对芳深 9、芳深 7、芳深 6井的天然气组成及甲烷同位素分析表明,松辽盆地北部昌德CO2 气为幔源无机气,该CO2 气是以由徐家围子连锁断层系下延与局部岩浆房相接作为通道,幔源热流底辟体中的CO2 气顺断层上移至合适的火山岩圈闭中而成藏

Huangqiao carbon dioxide gas field in North Jiangsu Basin have the following characteristics: deep gas fields are associated with shallow ones, marine gas fields are coupled with continental ones, and several gas reservoirs are combined. Carbon dioxide in Huangqiao area mainly comes from deep mantle, mixed with a little thermal metamorphism and a little organic carbon dioxide in shallow formation, and helium and nitrogen gas mainly come from mantle. There is a good time\|space matching relationship between carbon dioxide gas reservoirs and great rifts, magma and volcano activity, which forms the special carbon dioxide gas reservoir mode for Huangqiao. This mode has good sealing, trapping and preserving conditions, but its gas source differs from traditional hydrocarbon gas reservoirs.

苏北盆地黄桥CO2气田具有深部气田与浅部气田、海相气田与陆相气田匹配组合互成一体、多个气藏组合分布的特点,其CO2主要以深部幔源成因为主,浅层混有部分热变质成因和少量有机成因CO2,氦气和氮气主要为幔源成因,而且,黄桥地区CO2气藏的发育与深大断裂和岩浆火山活动具有很好的时空配置关系,形成了独特的&黄桥式&CO2气成藏模式,并具备良好的储盖圈保条件。

If these balls or "globs" of silica-rich magma are allowed to grow larger before the whole mass becomes solid, they can crack and shrink forming what later may become Thundereggs.

如果这些富有硅土的球状或水滴状岩浆,在整体大量变得坚实之前,增长的更大,那他们有能崩裂和收缩,以后或许会形成为雷公蛋。

With its swirling contours of gloopy, E-number orange, Magma Architecture's temporary installation to house an exhibition of the practice's work looks as though Angel Delight has been pumped into a room in the Berlinische Galerie, Berlin's museum of contemporary art, photography and architecture.

以它打旋的等高gloopy, E 数字桔子,岩浆建筑学的临时设施安置实践的工作的陈列看好像天使欢欣抽了入一个屋子在Berlinische Galerie,柏林的博物馆当代艺术、摄影和建筑学。

By means of distribution in figure of-La for the REE data, the original rocks of the garnet-pyroxene granulites would be derived from a mantle partial melting.

将REE数据投影到-La关系图中,投影点沿部分熔融斜线分布,提示原岩岩浆是地幔岩部分熔融产物。

In the dozens of million years, I watched it sometimes injected magma, burning everything into ash; sometimes ground and maintain shook, changing the route of rivers.

几千万年来,看到它时而在某处喷射岩浆,生灵涂炭;时而山摇地动,河川改向,但他依然是那个蓝色的美丽星球。

The notorious Dark Star Hellions and the Nova Demons are known for their piracy and murderous ways.

其中臭名招著的&黑星恶棍&和&岩浆魔&以他们盗抢和残杀的方式而闻名。

Geochemical characteristics indicate S-type granites and volcanic rocks depleted in sodium and enriched in potassium, with 62.42%~78.02% w(SiO2), 7.66%~9.13% w(K2O+Na2O), 1.18~2.62 w(K2O)/w(Na2O), and Rittmann index δ of 1.67~3.78. They are enriched in LREE with an average LREE/HREE ratio of 10.94×10-6, and generally depleted Eu with an minimum δEu less than 0.31 especially in the ignimbrite and biotite granite, which have experienced a significant process of separation and crystallization of plagioclases.ΣREE at the main stage of the magmatic activity decreases with time.

地球化学特征显示矿区火山——侵入岩属于贫钠富钾的S型花岗岩,其w(SiO2)值为62.42%~78.02%、w(K2O +Na2O)值为7.66%~9.13%、w(K2O)/w(Na2O)比值为1.18~2.62、里特曼指数δ为1.67~3.78;矿区岩石LREE/HREE比值平均为10.94×10-6,属于轻稀土富集型;Eu普遍亏损,特别是熔结凝灰岩、黑云母花岗岩δEu<0.31,表明经历了显著的斜长石的分离结晶作用;自早至晚主阶段岩浆活动稀土总量逐渐降低。

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