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1)  mantle-derived fluids
幔源流体
2)  mantle gold bearing fluid
幔源含金流体
1.
The mechanism of positive emplacement of mantle gold bearing fluid is proposed on the basis of the composition of quartz inclusions,theoretical analysis of forming mechanism of ore controlling struc tures,high T,P experiments and dynamic mathematical formulae,instantaneous emplacement of gold bearing fluid and forming setting of ore controlling structures.
基于石英包裹体成分测定、容矿断裂形成机制的理论分析、高温高压实验研究、动力学数学公式举例、含金流体瞬间就位过程及容矿断裂形成环境的探讨 ,提出了幔源含金流体主动就位机制。
3)  mantle-derived fluids flow
幔源流体活动
1.
The Gaoqing-Pingnan fault is the primary pathway of mantle-derived fluids flow in the Dongying sag.
高青-平南断裂带幔源流体活动方式和活动强度存在着时间和空间上的差异,该断裂带在古近纪-新近纪至少经历了四期富CO2幔源流体活动。
4)  mantle-derived xenoliths
幔源包体
1.
Laser-fluorination technique has been used to determine the O-isotopic ratios of mineral separates from mantle-derived xenoliths from the Yitong.
吉林伊通幔源包体的氧同位素组成徐义刚,M。
5)  mantle xenolith
幔源包体
1.
Clinopyroxene-melt equilibrium temperature and pressure of Cenozoic basalts with special reference to the genesis of mantle xenoliths in some areas of eastern China;
中国东部几个地区新生代玄武岩中单斜辉石-熔体平衡温压——兼论幔源包体的成因
2.
The Quaternary basalts in Shandong Province contain mantle xenoliths of varied quantities and sizes.
山东省第四纪玄武岩中含有数量、大小不等的幔源包体。
3.
The mantle xenoliths collected from these three localities have been described in this paner.
中国东部含幔源包体的早第三纪玄武岩已发现的有吉林双辽、河北阳原和山西繁峙。
6)  mantle xenoliths
幔源包体
1.
In eastern China there are more than one hundred reported localities of mantle xenoliths, on which a lot of studies have been carried out.
新生代火山岩中的幔源包体可以提供有关上地幔的直接信息。
2.
The upper mantle geotherm and rheology for Mingxi, Fujian Province, has been constructed through a detailed study of mantle xenoliths collected from this area.
通过对采自福建明溪的幔源包体样品的详细研究,建立了该区上地幔的地温线,探讨其流变学特征。
3.
Major, trace element composition and Sr-Nd-Pb isotopes of the Cenozoic basalts from Yangyuan (Hebei Province) and Datong (Shanxi Province), which are located to west of the Daxinanling-Taihanshan gravity lineament, as well as mineral chemistry, major and trace element composition and Sr-Nd isotopes of mantle xenoliths from Yangyuan are reported in this thesis.
本文报道了大兴安岭-太行山重力梯度带以西河北阳原和山西大同新生代玄武岩的元素和Sr-Nd-Pb同位素地球化学及阳原幔源包体的矿物化学、元素和Sr-Nd同位素地球化学,据此对华北克拉通西部上地幔的性质和过程进行了初步讨论。
补充资料:《满洲源流考》
      中国清代官修满族先世及其有关东北诸民族的重要史籍。清高宗弘历于乾隆四十二年(1777)谕,将"建州之沿革、满洲之始基,与夫古今地名同异","详加稽考、勒为一书"。大学士阿桂(1717~1797,正蓝旗满洲人)、于敏中(1714~1779,江苏金坛人)等奉敕撰。翌年书成,共20卷。内容分4门:①部族(卷1至卷7),上溯肃慎以及挹娄、勿吉、靺鞨、完颜诸部和相邻近的索伦、费雅喀等部的兴衰,稽核史籍,考订异同。②疆域(卷8至卷13),始自肃慎,迄至元时,凡史册所载诸城镇村寨,按其方位,证以当时地理形势,分条辨释,并将辽、金宫室建置和古迹载入,附以明卫所城站考。③山川(卷14至卷15),对其名川胜地据地志所载,古今互证,析异定讹,不可考者存疑。④国俗(卷16至卷20),对满族及其先民的习俗、祭祀、物产等分条胪列,并就骑射的起源和饮食特点等方面繁征博引;还以渤海的文献、金源的官制,附录于此。此书系清统治者为炫耀其先世渊源久远、部族众多的发祥历史而作,对女真各部与明王朝的隶属关系,力加隐晦;对于建州三卫,尤有所讳,略而不论。但是,由于书中全面地系统地搜辑了有关文献资料,仍不失为研究东北史地和满族等诸民族的重要参考资料。
  
  
  

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