magmatic evolution meaning in Chinese
岩浆进化作用
岩浆演化
岩桨进化
Examples
- The main aim of study on volcanic rocks of orogenic belts is to retrace the history of tectono - magmatic evolution of orogenic belts
摘要造山带火山岩石学研究的主要目的在于重溯造山带-岩浆演化历史。 - They all belong to the calc - alkaline island arc series and are closely related to the evolution of the arc - basin systems of the gangdise tectonic belt . based on studies of petrology , litho - geochemistry , tectonic setting , petrogenesis and magmatic evolution , the present dissertation summarized the general evolutionary regularity of the magmatic rocks in time and space . the magmatic rock assemblages are divided into the inter - arc spreading basin t
在对研究区主要矿产分布特征、成因类型系统分析的基础上，总结了措勤地区构造岩浆演化与成矿的关系，并将研究区成矿系统划分为汇聚大陆边缘成矿巨系统、碰撞造山成矿巨系统和陆内汇聚成矿巨系统。 - On the basis of the an integrated study on strata , magmatic - volcanic activities , geochemistry as well as geophysics and remote sensing imagines , three subtectonic units were divided . 2 , metallogenic series of copper deposits with the elapse of time , the tectonic - magmatic evolution went on from south to north , which resulted in regular production and spatial distribution of ore resources , correspondingly forming east tianshan copper , gold , nickel , iron , silver clucters of mineral deposits . in the light of the concept of metallogenic series by cheng yuqi , chen yuchuan et al . ,
本文立足于东天山地区铜及其多金属矿床的野外地质调查研究，从充分整理和吸收消化前人大量研究成果的基础之上，选择重点矿床进行解剖，辅以岩石学和高精度同位素年代学研究，尝试应用成矿系列理论来认识东天山地区铜矿床的时空分布和演化谱系，以内生金属矿床时空分布样式作为大地构造环境的标志和限定，为东天山大型铜矿富集区的战略靶区优选提供理论依据。 - We might retrace the history of tectono - magmatic evolution of volcanic magmatism at different stages of formation - evolution of orogenic belts and further explore some important scientific problems of global dynamics and comparative planetary dynamics by means of comparison in larger scales
因此，我们可以根据造山带形成演化不同阶段火山岩浆作用的特点来重溯造山带的构造-岩浆演化历史，并进而从更大尺度上加以对比，探索全球动力学乃至比较行星动力学等重大科学问题。