火山弧的英文

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"火山弧"怎么读用"火山弧"造句

英文翻译手机版

volcanic arc

"火山"英文翻译 volcano; burning mountain
"弧"英文翻译 arc bow
"内侧火山弧" 英文翻译 : inner volcanic arc
"山弧" 英文翻译 : mountain arc; mountainarc
"次生山弧" 英文翻译 : secondary mountain arc
"挤压造山弧" 英文翻译 : compressional orogenic arc
"弯曲山脉；山弧" 英文翻译 : orocline
"袖山弧线" 英文翻译 : sleeve ca curve; sleeve cacurve line
"俾路支山弧" 英文翻译 : baluchistan arc
"火山" 英文翻译 : [地质学] volcano; burning mountain 活火山 active volcano; 死火山 extinct volcano; 休眠火山 dormant volcano; 火山爆发 volcanic eruption; 火山玻璃 volcanic glass; 火山沉积 volcanic deposit; 火山尘 volcanic dust; 火山带 volcanic belt; 火山地震 volcanic earthquake; 火山构造 volcanic structure; 火山坑 fire pit; 火山熔岩 slag; 火山锥 volcano; cone
"渐缩环形山弧" 英文翻译 : decremental arc
"相接环形山弧" 英文翻译 : contiguous arc
"火山道；火山口" 英文翻译 : volcanic vent
"火山火山" 英文翻译 : volcano
"火山雷火山雷" 英文翻译 : volcanic thunder
"火山碑；火山塔；火山柱" 英文翻译 : volcanic spine
"冰火山" 英文翻译 : cryovolcano
"侧火山" 英文翻译 : lateral volcano; parasitic volcano
"雏火山" 英文翻译 : embryonicvolcano; volcanic embryo
"单火山" 英文翻译 : isolated volcano; simple volcano; simplevolcano
"岛火山" 英文翻译 : island volcano
"盾火山" 英文翻译 : shield volcano
"副火山" 英文翻译 : satellite volcano
"复火山" 英文翻译 : complex volcano
"古火山" 英文翻译 : ancient volcano; palaeovolcano

例句与用法

Their structural environment is mainly volcanic arc
其构造环境主要为火山弧地区。
Study on petrology , geochemistry and isotope chronology shows that the metallogenesis is closely related to granite - porphyry , which belongs to the early ordovician adakite formed in volcanic arc
花岗斑岩与成矿作用关系密切，从岩石学、岩石化学、年龄学等方面对花岗斑岩进行了研究，认为花岗斑岩属于志留世早期形成于火山弧环境的埃达克岩。
At last they have being formed the tectonic framework , after breakup of the volcanic island arcs , subduction , decline and fall of the back - arc basins and arc - microcontinent and arc - arc collision had finished
经过了长期而复杂的微大陆和火山弧的裂解、弧后盆地的消减衰亡及弧陆和弧弧碰撞等构造演化，才最终形成今天所见到的这种构造样式。
And apatite . by these analyses and comparison with general granite both in china and the world and with the granite in other au or cu belt in china , the characteristics of the granite in this area are concluded as follows . it belongs to magnetite - i or syntectic granite and has crust - mantle mixed characteristics ; it was formed mainly by crystallization differentiation of melting magma and multiphase varied intrusion ; the degree of differentiation evolvement is not high ; the granite and its enclaves p . re congenetic ; the range of temperature is about 500 - 700 , the range of pressure is about 2 . 50 gpa - 4 . 35 gpa , and the range of oxygen fugacity ( lg fo2 ) is - 15 . 53 - - 14 . 00 ; most granite bodies formed before the collision of plates , and few formed after the collision of plates
通过对测试数据的分析与综合研究，并同中国和世界一般花岗岩类以及中国主要金、铜成矿岩体的花岗岩类进行对比，得出本区花岗岩类岩石具有以下特征：属磁铁矿-型或同熔型花岗岩，其岩浆物质具壳幔混源特征：主要由熔融态岩浆经结晶分异作用，通过多期变速上侵而形成；其分异演化程度较低；寄主岩基和包体具有同源性；岩石的形成温度范围约为500 - 700 ，压力大约为2 . 50gpa - 4 . 35gpa ，氧逸度值1gfo _ 2为- 15 . 53 ? 14 . 00 ；该岩带主要形成于板块碰撞前消减的活动板块边缘期，为燕山至喜马拉雅早期的大陆边缘火山弧环境的产物。