- 更多网络例句与火山作用相关的网络例句 [注：此内容来源于网络，仅供参考]
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At the stage of geosyncline, the huge thick sal geo synclinal structural layer would be formed by volcanism and weathering deposition; the Caledonion granites would be form ed by remelting or mix-melting.
地槽阶段，火山作用及风化沉积作用等形成了巨厚的硅铝质地槽构造层；重熔或混熔（包括混合作用和/或同化混染作用）形成了加里东花岗岩类。
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Magmatism in the form of volcanism and plutonism is predominant in the diwa maximummobility period which results in thick volcanic rock and all big intrusive bodies in the area.
岩浆作用(包括火山作用和侵入作用)在北京西山地洼激烈期中有强烈的表现，形成区内巨厚的火山堆积和大规模的侵入体。
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Sub-volcanic rocks include andesitic porphyrite, rhylitic porphyry, cryptoexplosive breccia as well as autobreccia etc.(2) Volcanic lithofacies——through the observation of cores, identification of thin sections and interpretation of well logs and seismic data, there are 8 kinds of lithofacies for the volcanic rocks of Yingcheng Formation are identified: fallout facies, effusion facies, pyroclastic flow facies, base surges facies, lahar facies, eruption-sedimentary facies, subvolcanic facies and extrusion facies.(3) Three types of eruption——i. e. explosion, effusion and surge.(4) Two kinds of eruptive environments——Subaerial (e. g. volcano in Well Shangshen 3) and subaqueous .(5) Three remarkable volcanic apparatus in Shengping-Wangjiatun area——layered, micro-shield and cone volcanoes according to volcanic processes and lithofacies distribution.
次火山岩有安山玢岩、流纹斑岩、隐爆角砾岩及自碎角砾岩等；(2)火山岩相——通过岩芯观察、镜下鉴定、测井与地震资料解释，营城组火山岩中发育8种岩相类型，即爆发空落相、溢流相、火山碎屑流、基底涌流相、喷发沉积相、火山泥石流相、侵出相和次火山相等；(3)火山喷发的形式——有爆发、溢流和涌流三种；(4)火山喷发环境——有陆上(如尚深3井火山)和水下两种；(5)火山机构类型——根据火山作用特点和岩相分布特征，在升平—汪家屯地区识别出三类截然不同的火山机构，即层火山、微型盾火山和渣锥火山。
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Since it is a volcanic park, there are lots of illustrations describing the history and the force of volcanism.
由於它是个火山公园，因此就有许多的标示来说明火山作用的影响和历史。
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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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Veined,stockwork and alteration-sheathed gold ores have been found in the area,belonging to four genetic types:the volcanic hydrothermal ores related to early—middle Carboniferous volcanism; subvolcanic hydrothermal ores related to intermediate—acidic porphyry intrusions; hydrothermal ores to the granitic intrusion and dynamo- hydrothermal ores related to regional dynamic metamorphism along the faults.
矿石类型有含金石英大脉型、石英网脉型和蚀变岩型。矿床成因类型有4种：一为火山热液型，其成因与区内早—中石炭世火山作用有关；二为潜火山热液型，与中酸性斑岩体侵位有关；三为岩浆热液型，与花岗质岩浆的侵位有关；四为动力变质热液型，沿断裂带分布于蚀变玄武岩中，系区域动力变质作用的产物。
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Veined,stockwork and alteration-sheathed gold ores have been found in the area, belonging to four genetic types: the volcanic hydrothermal ores related to early-middle Carboniferous volcanism; subvolcanic hydrothermal ores related to intermediate-acidic porphyry intrusions; hydrothermal ores to the granitic intrusion and dynamo- hydrothermal ores related to regional dynamic metamorphism along the faults .
矿床成因类型有4种：一为火山热液型，其成因与区内早-中石炭世火山作用有关；二为潜火山热液型，与中酸性斑岩体侵位有关；三为岩浆热液型，与花岗质岩浆的侵位有关；四为动力变质热液型，沿断裂带分布于蚀变玄武岩中，系区域动力变质作用的产物。
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Type-B Nodule: The source of elements in the nodules comes from slow deposition of the overlying water and the diffusion of the pore water, which comes mainly from the double decomposition reaction of Fe, Mn oxides caused by the oxidation diagenesis of organic material in sediment and its forming process and distribution is controlled by pH in the pore water. There is no corrlation between distribution of the nodules and water depth, topograph.
A型结核主要分布于深海火山沉积环境区，受上覆水Mn〓和Eh制约；B型结核一方面由于在深海火山沉积环境区，受生物作用影响，另一方面在生物沉积环境区，又受火山作用影响，使此类结核的分布与大洋地貌和沉积物的关系不明显；C型结核主要分布在太平洋CCD范围内，受沉积环境上生物和活性有机碳的制约。
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The clay mineralogy composition and clast composition difference between different section or different levels in one section may result from variable intension of the volcanism, distance from the volcanism center and paleogeographical location.
同是深水相P-T界线剖面附近的黏土岩以及同一剖面不同层位的黏土岩中的黏土矿物和碎屑物质存在较大的差异，其原因可能是与火山作用的强弱、离火山活动中心的远近以及所处地理位置有关。
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There are 4 end members of volcanic clasts, including catapult airfall, ejection airfall, base surge and volcanic clasts flow.
与火山作用有关岩相有4种端元的火山碎屑岩相：弹射坠落爆发空落相、喷射降落爆发空落相、热碎屑流相和热基浪相。
- 更多网络解释与火山作用相关的网络解释 [注：此内容来源于网络，仅供参考]
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extrusive vulcanicity：喷出火山作用
extrusive rock喷出岩 | extrusive vulcanicity喷出火山作用 | eye of tropical cyclone(热带气旋)
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volcanicity：火山活动 火山作用
volcanicislandarc 火山岛弧 | volcanicity 火山活动 火山作用 | volcaniclastic 火山碎屑的
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volcanicity：火山作用
"火山导管","volcanic vent" | "火山作用","volcanicity" | "火山碎屑的","volcaniclastic"
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volcanism：火山作用
至於说到什麼是火山学(Volcanology)﹖当然要知道什麼是火山作用(Volcanism). 地球内部产生的高温熔融流体称之为岩浆,这些岩浆遇到地壳脆弱处或裂隙带时,将伴随著水气一起冲破地壳而喷出地表,造成各种火山活动.
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epigenetic volcanism：后期火山作用
epigenetic structure 表皮构造 | epigenetic volcanism 后期火山作用 | epigenetic volcano 后期火山
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epigenetic volcanism：后期火山作用,后成火山作用
表皮构造,浅层构造 epigenetic structure | 后期火山作用,后成火山作用 epigenetic volcanism | 后生水,再生水 epigenetic water
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sedimentary volcanism：沈积火山作用
沈积盆地 sedimentary trap | 沈积火山作用 sedimentary volcanism | 沈积作用 sedimentation
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vulcanicity：火山作用
火山作用 volcanic action | 火山作用 vulcanicity | 火试法 pyrognostic test
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vulcanism：火山作用
vulcanian 火山的 | vulcanism 火山作用 | vulcanite 硬橡皮
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volcanism; vulcanism：火山作用;火山活动
火山碎屑岩 volcaniclastic rock | 火山作用;火山活动 volcanism; vulcanism | 歪长辉熔岩 volcanite