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The circulation of volcanic hot spring formed the alteration zone which, together with atmospheric water and subvolcanic hydrothermal solution, formed micro-crystalline quartz that contained adular and sericite.

火山热泉循环形成蚀变晕,此阶段有大气降水的参与;潜火山热液成矿阶段发育的低温微细石英网脉中含冰长石和绢云母。

The petrophysical properties of volcanic rock reservoirs in Junggar Basin are generally characterized by the following: the acidic lava and auto brecciated lava are the best, especially the petrophysical properties of auto brecciated lava and andesites after the tectonic movement and denudation process in the later stages are superior to those of basalts.

准噶尔盆地火山岩储层物性一般特点是:酸性熔岩、火山角砾岩最好,特别是经后期构造运动和溶蚀作用改造后的火山角砾岩;安山岩的物性总体优于玄武岩。

The petrophysical properties of volcanic rock reservoirs in Junggar Basin are generally characterized by the following: the acidic lava and auto brecciated lava are the best, especially the petrophysical properties of auto brecciated lava and andesites after the tectonic movement and denudation process

准噶尔盆地火山岩储层物性一般特点是:酸性熔岩、火山角砾岩最好,特别是经后期构造运动和溶蚀作用改造后的火山角砾岩;安山岩的物性总体优于玄武岩。

A pool of mud boils near Dallol Volcano, located in Ethiopia's remote Danakil Depression.

一滩沸腾的泥浆在Dallol火山周围,火山地处埃塞俄比亚偏僻的Danakil低地。

The hypo-volcanic crytoexplosion Breccia rock body is formed of granite magma, which is rise to the lower of the earth s crust along the east-western shear zone and exploded below the Archean fundus rock. The felstone vein and the hypo-volcanic crytoexplosion Breccia rock are from the same magma source, and are formed in the different evolution stages.

香炉碗子金矿区分布的次火山隐爆角砾岩体是由花岗质岩浆沿东西向脆~韧性剪切带上升到地壳浅部隐爆太古代基底岩石所形成,霏细岩脉与次火山隐爆角砾岩来自同一岩浆源,为同一岩浆活动不同演化阶段所形成的。

The early stage of the Yanshan movement generated an Early Jurassic downfaulted basin and a Middle Jurassic compressional-downwarped coalaccumulating basin.In the middle stage,the Mid-Late Jurassic witnessed the formation of a volcanic downfaulted basin bounded by NW and NE deep faults,intermediate-basic and acid volcanic eruption and hypabyssal and near-sur...

燕山运动早期形成早侏罗世断陷盆地和中侏罗世挤压坳陷型聚煤构造盆地;中期中晚侏罗世形成被NW、NE向深大断裂围限的火山断陷盆地,中基性—酸性火山喷发和浅成、超浅成中酸性岩浆侵入,晚侏罗世末形成了一系列NNE向褶皱和逆冲推覆构造带;晚期早白垩世再次形成断陷盆地和开阔平缓褶皱,义县组不整合在火山岩之上,晚白垩世处于挤压造山后的山体隆升阶段,左云组不整合在义县组之上,伴随有壳源型花岗岩侵入,NW、NE向断裂复活,形成地堑、地垒式断裂组合,导致山体隆升。

Iron deposit is concerned with spilite keratophyre, rich in Fe, Na〓O, Alternative types are similar-skarnization, Iron deposit is of aeromagnetic anomaly. Indexes of Cu, Pb-Zn deposits are contemporaneous fault, ore-bearing bed, volcanic rock with high potassium, volcanic structure, a serious of alternative in ore-bearing bed and under ore-bearing bed, high content of Pb, Zn, Ag, Cu, Cd, Ba, As, CaO, Fe, Mn, low Na〓O, Al〓O〓 in mineralizing body.

铅锌矿形成大矿富矿指标:①NW、NE向同生断裂;②有利含矿层位D〓k〓〓;③酸性富钾火山岩;④火山机构发育;⑤有利于矿质聚集的火山洼地;⑥发育与流体活动有关的矿下层、矿层、蚀变岩筒蚀变;⑦块状、浸染状铅锌黄铁磁黄铁矿石;⑧原生晕中Pb、Zn、Ag、Cd、Ba、Cu、As元素组合,CaO、TFe、Mn富集,Na〓O、Al〓O〓亏损,其下部位富K〓O或Na〓O。

And therefore the Jinchang gold deposit can be classified as the catalog of mesothermal gold deposits which are related to post-magmatic hydrothermal activity of Mesozoic volcano-subvolcanic magmatism.

矿石中脉石英的Ar-Ar年龄测定结果(119.40~122.53Ma),表明矿化作用发生于燕山中晚期,矿床成因为与中生代火山-次火山活动有关的岩浆期后浅成中温热液矿床。

The author has paid attention to the two kinds of lavas which locate the south-east end of the Kalamaili belt. Through the field investigate and the geochemistry experiment the author has contrasted the two kinds of lavas in the ophiolitic melange, made clear the tectonic background and summarized the geochemical characteristic and then discussed the formed environment and tectonic significance.

作者以该蛇绿混杂岩中的两类中基性火山熔岩为研究对象,通过野外实际观察和室内地球化学实验分析,将这两类火山熔岩进行对比研究,弄清其大地构造背景,总结其地球化学特征,并由此探讨该蛇绿混杂岩的形成环境及其构造学意义。

Considering near field observation and parameter interp retation of source mechanics, the authors think that the low or higt velocity be lts in Tengchong volcano areas are closely related to the magma activities of th e volcanoes.

根据本文成析成象结果,结合数字化近场地震观测资料及震源力学参数特征解释,分析认为,腾冲火山区地壳不同深度存在的低速带或高速带均与火山作用的岩浆活动有密切关系。

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