volcanic gas 中文意思是什麼

volcanic gas 解釋
火山氣體
  • volcanic : adj. 1. 火山(性)的;火山作用形成的,火成的。2. 有火山的,火山多的。3. 暴發性的,猛烈的,激烈的。adv. -ically
  • gas : n (pl gases )1 氣,氣體,氣態 〈cf fluid; solid〉 2 可燃氣,煤氣,沼氣;【礦物】瓦斯。3 【軍事...
  1. Volcanic tremor is due to the oscillation of magmatic gas or due to the crater-wall downfall.

    火山地震由火山氣體振蕩或火山口內壁崩塌引起。
  2. Sensors on the slopes of the two mountains - anak krakatoa on the southern tip of sumatra and tangkuban prahu in java - picked up an increase in volcanic activity and a buildup of gases, government volcanologist syamsul rizal said on wednesday. on tuesday, mount talang, also on sumatra, sent clouds of gas high into the air

    印尼火山學家上周三說,安放在蘇門答臘島南端的喀拉喀托火山和爪哇島上的唐庫班珀拉胡火山山坡上的傳感器檢測到這兩座火山的活動在加劇,而且氣體也在積聚。
  3. Volcanic hydrothermal activities and gas - releasing characteristics of the tianchi lake region, changbai mountains

    長白山天池火山水熱活動及氣體釋放特徵
  4. Characteristics of mesozoic volcanic rocks and its controlling effect on gas reservoir in songliao basin

    北部灣盆地潿洲組復合扇體特徵及油氣勘探意義
  5. Volcanic tremor is due to the oscillation of magmatic gas or due to the craterwall downfall.

    火山地震由火山氣體振蕩或火山口內壁的崩塌引起。
  6. In the ensuing excitement, researchers advanced many theories to explain them : leaking aquifers ( which would be inexplicably perched high on crater rims ) ; pressurized geysers of water ; high - pressure outbursts of carbon dioxide gas ; volcanic heat sources at depth

    在接下來的一陣狂熱中,研究者提出許多的理論來解釋: ?漏的含水層(在隕石坑外緣必須被抬升至非常高的高度) 、受壓的間歇泉、高壓噴出的二氧化碳氣體、深層的火山熱源等。
  7. It is therefore proposed in this paper to strengthen the exploration of such wide and deep subsags as chagannuoer and hongqi subsags, to lay emphasis on the exploration of superposed and residual fault depression, and to pay attention to the discovery of various oil and gas reservoirs including metamorphic buried hills, fracture slope breaks, and volcanic rocks, etc

    因此,指出下一步應加強類似查干諾爾,紅旗等寬深窪槽的勘探,重視具疊合型和殘留型斷陷的勘探,注重尋找包括變質巖潛山,斷裂坡折帶、火山巖等在內的各類油氣藏。
  8. The relationships between the accumulation of gas hydrates and the typical diapirs in passive continental margin are summarized in primary in this paper which suggest that the factors in passive continental margin including the thick sediment layers, plastic substance, high pressure fluid, outboard volcanic activities and the process of stretch - rupture provide favorable conditions for the formation of the diapirs which can form advantageous environment for gas hydrates coming into being

    初步總結了被動大陸邊緣中典型底辟構造與天然氣水合物的成礦關系,認為被動陸緣內巨厚沉積層、塑性物質與高壓流體、陸緣外側的火山活動及張裂作用,為底辟構造發育提供了條件,形成了水合物成礦的有利空間。
  9. Through comprehensive analysis, we found that there are 6 thermal fluid activities and 4 charging periods of gas in the volcanic reservoir of the yingcheng formation in xujiaweizi rift

    根據成分的不同可將本區的次生包裹體分為鹽水包裹體和含烴鹽水包裹體,其中含烴鹽水包裹體所佔的比例要遠小於盆水包裹體。
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