查询词典 eruptive
- 与 eruptive 相关的网络例句 [注:此内容来源于网络,仅供参考]
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The scene of the geo-park is rich in volcanic rocks, which predominately consists of pyroclast-bearing and volcanoclastic rocks with porphyritic texture and can be classed into plutonic, epizonal, intrusive, extrusive and eruptive environments.
通过对大别山金刚台国家地质公园火山岩的岩性特征、火山岩相、相模式和火山机构的研究,认为火成岩斑状结构的含碎屑碎屑状岩石可以有深成、浅成、侵出、喷溢或爆发等不同产状。
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A small indented scar left in the skin by smallpox or other eruptive disease; a pockmark.
痘凹小坑似的疤,因得天花或其他暴发性疾病而留在皮肤上的;痘凹
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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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If the result makes clear,be before flu is eruptive, people has a kind of mysterious appetite to quick-freeze bramble, flu trend report of Gu Ge is met in studying this kind to be added to algorithm.
如果结果表明在流感暴发前,人们对速冻树莓有一种神秘的食欲,谷歌的流感趋势报告就会把这种研究添加至算法中。
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A good many mico-landblock of the early Neoproterozoic-Cambrian volcanic rock that distribute in the Tianshan orogenic belt and on its both sides, and the Carboniferous-Permian volcanic rocks that widely distribute in the Tianshan and adjacent regions are selected for subject investigating in this paper. Renewing the ocean-land format and ocean-land conversion process of Tianshan orogenic belt in the Paleozoic is the masterstroke for this paper. On the basis of detailed field investigation, many subjects, such asregional lithology、geochemistry、structural geology、volcanic sedimentology geology、sotope geochronology and synthesis analysis study of geophysics data, are adopted as instrumentality in the paper, this study lays emphasis on the formation, evolution and dynamics of early Neoproterozoic-Cambrian and Carboniferous-Permian volcanic rock in the Tianshan and its adjacent regions to find out Carboniferous-Permian volcanic rock property, eruptive sequence, time and space distribution characteristics, to resume and reconstruct evolution process of Carboniferous-Permian volcanic rock, and to explore connection of magmatism process and lithosphere stretching action of neopaleozoic ocean-land transformation in the Tianshan region.
本文选择分布于天山及其两侧的诸多微陆块上新元古代—早寒武世火山岩和天山地区广泛发育的石炭纪—早二叠世火山岩为研究对象,以恢复重建天山造山带古生代洋陆格局和洋陆转换过程为主线,在详细的野外工作基础上,综合运用区域岩石学、地球化学、构造地质学、火山沉积学、同位素地质年代学、区域地球物理资料综合分析研究等多学科手段,重点研究天山及其邻区新元代—早寒武世和石炭—二迭纪火山岩系的形成演化及其动力学,查明天山石炭纪火山岩系的性质、喷发序列、时空分布特点,恢复重建其形成演化过程,探索天山地区晚古生代洋陆转换过程中火山岩浆作用与岩石圈拉伸作用的关系。
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This study shows that there are 4 kinds of volcanic facies in deep volcanics in north Songliao Basin: eruptive facies, overflow facies, volcanic vent facies and volcanic sedimentary facies. There are 4 volcanic eruption cycles: Huoshiling period, Shahezi period, Yingchengzi period and Quantou period. There are 4 structural evolution stages: north-south accumulation, west-east subduction, uplift mantle and thin crust, alternative open and close. There are 4 kinds of pool-forming patterns:(1) pattern with the migration along the unconformity and fault to the near crater;(2) pattern with the migration along unconformity and fault to the rift margin;(3) pattern with the migration along unconformity, fault and fracture to the source rock;(4) pattern with the migration of the deep gas along the deep and large fault to the volcanic trap.
研究认为,松辽盆地北部深层火山岩主要存在四种火山岩相:即爆发相、溢流相、火山通道相、火山沉积相,划分为四个火山喷发旋回:即火石岭期、沙河子期、营城子期、泉头期,经历了四个构造演化过程:即南北夹攻、东西俯冲、幔隆壳薄、开合交替,具有四种成藏模式:即沿不整合面和断层运移至近火山口处火山岩圈闭聚集成藏模式、沿不整合面和断层砂岩疏导层运移至断陷边部火山岩圈闭聚集成藏模式、沿不整合面及断层、裂缝运移至源岩区内凹中隆火山岩圈闭聚集成藏模式、深部无机成因天然气沿深大断裂运移至火山岩圈闭聚集成藏模式。
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While porokeratosis is practically asymptomatic,unusual pruritic variant has been reported and designated as "eruptive pruritic papular porokeratosis" or "inflammatory stage of DSP".
本病一般无临床症状,但伴明显瘙痒的汗孔角化症已经有文献报告,并被命名为&发疹性瘙痒性丘疹型汗管角化症&或&处于炎症反应期的DSP&。
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We recently encountered three old men with pruritic porokeratosis .We propose the term "eruptive pruritic papular porokeratosis" for describing this unusual variant of porokeratosis.
笔者近期诊断三例这样的病患并推荐使用&发疹性瘙痒性丘疹型汗管角化症&来命名这一特殊类型的汗孔角化症。
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A pitlike scar left on the skin by smallpox or another eruptive disease.
一个希望的突然失落会留下一处伤痕,即使那希望最终会实现,也决不能完全平复--托马斯·哈代
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The central scenic area is the entire garden heart, collection each kind of activity is a body, take the main body architectural complex as the division space, by flower-bed, presbyopic glasses, rockery, eruptive fountain, sculpture and so on rich level, by hundred scenic spot compositions and so on gardens, vineyard, library, exhibition hall, garden, porch pavilion.
中心景区是全园心脏,集各类活动为一体,以主体建筑群为划分空间,以花坛、花镜、假山、喷泉、雕塑等丰富层次,以百花园、葡萄园、图书馆、展览馆、庭院、廊榭等景点组成。
- 推荐网络例句
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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.
最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。
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Only person height weeds and the fierce looks stone idles were there.
只有半人深的荒草和龇牙咧嘴的神像。
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This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.
这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。