海底热泉 meaning in Chinese
hot spring
Examples
- Fankou pb - zn deposit is a submarinehydrothermal spring effusion type ore deposit , which occurred in upper paleozoic carbonaterock formation
凡口铅锌矿床是发育于上古生界碳酸盐岩建造中的海底热泉喷溢矿床。 - What is more , all the reactants in this experiment ? a thiol , carbon monoxide and water ? are readily available near sulfide - rich hydrothermal vents
此外，这项实验使用的反应物质如硫醇、一氧化碳和水，在硫化物丰富的海底热泉十分常见。 - Perhaps , brandes thought , the environment at hydrothermal vents mimics an industrial process in which ammonia is synthesized by passing nitrogen and hydrogen over a hot metallic surface
工业上可以在高热金属表面通过氮气与氢气以合成氨，于是布兰德斯便推想，也许海底热泉附近环境与工业制程有类似的地方。 - The ore - bearing fluid of dabaoshan deposit was relate to magmatic thermal dynamic process and formed hydrothermal sedimentary polymetallic deposit at seafloor . the ore - bearing fluid of fankou was relate to circulation hydrothermal fluid in deep formation and formed pb - zn - ag - hg polymetallic middle - lower temperature sedimentary deposit by sea - floor thermal spring overflowing
大宝山型流体与岩浆热动力作用有关，形成海底火山热液沉积多金属矿床；凡口型流体与深部建造的循环热液有关，形成中低温海底热泉喷溢沉积铅锌银汞矿床；红岩型流体与盆地成岩压实水有关，形成低温单一黄铁矿矿床。 - By analyzing and generalizing minerogenetic and geological background , mineral constituent , rare - earth element , isotope and typomorphic feature of sulpurization mineral , finally , we made a conclusion that fankou desposit resulted from the hot spring eruption at the bottom of sea , it has a character of syngenetic sedimentary deposit , which was affected by the late hydrothermal superimposed and light rebuilding after it came into being , which is typical sedex bedded - controlled deposit
通过对凡口矿床的成矿地质背景、矿物成分、稀土元素、同位素以及的黄铁矿、闪锌矿、方铅矿标型特征进行了分析总结，确定了凡口矿床是海底热泉喷溢形成的，同时又受到后期热液轻微叠加改造，属于典型的sedex型层控矿床。