n.成矿作用
metallography───n.[材]金相学
metallotherapy───n.金属疗法
metallographist───n.金相学家
metallochromy───n.金属染色，金属表面染色
metalloid───n.非金属；[材]类金属；准金属；adj.非金属的；类似金属性的；准金属的
metallographic───adj.金相学的，金相的
metallorganic───有机金属的
metalloidal───类金属
metallochrome───n.金属着色剂
metallographic experiment───金相实验
The geodynamic regime of mantle-derived uranium metallogenesis and theory of hotspot uranium metallogenesis are briefly discussed.───了幔源铀成矿的地球动力学背景，评述了热点铀成矿理论。
Outwards from the mantle uplift center, the metallogenesis becomes weaker, the deposit scale smaller and the ore-bearing horizon older.───该矿带具有自幔隆中心向外矿化渐弱、矿床规模变小、赋矿层位变老等规律。
This process is called tectonic-metallogenesis.───这一过程被称为构造成矿作用。
Geological data and experimental data demonstrate that: ore-controlling faults are simultaneity-metallogenesis faults in this deposit.───实际地质资料和模拟实验研究都表明，该矿床控矿断裂为同成矿断裂。
What have been doing above have actual meanings for evaluating uranium metallogenesis of Erlian basin.───这对评价二连盆地的铀成矿远景具有现实意义。
The experiments also show that the tectonic overpressure is an important condition for gold metallogenesis in the study area.───构造附加压力是促进该区金成矿的重要动力条件。
This paper deals with the metallogenesis direct related to the regional prospecting evaluation.───本文着重探讨了与区域汞矿找矿评价直接相关的成矿问题。
The metallogenesis is strictly controlled by NE- trending shear fault zone.───成矿严格受NE向剪切断裂带控制。
Deep and large fault system played an important role in lithogeny and metallogenesis.───深大断裂在成岩成矿中占重要地位。
Geological data and experimental data demonstrate that: ore - controlling faults are simultaneity - metallogenesis faults in this deposit.
The inner, outside contact zone between Himalayan ultra-epizonal syenite porphyry, Indosinian volcanic rocks of liparite porphyry-dacite series and strata is very advantageous to the metallogenesis.
The alteration and metallogenesis of Pulang porphyry Cu deposit are rather typical.
In the end, the relation between the metallogenesis and the evolution of Archaeozoic and Early Proterozoic earth crust is discussed basing upon the theory of rift.
In the ore field, the mineralization and alteration is intensive distributed in the wall rocks. The skarn alteration, silicification and epidotization are most correlative to metallogenesis.
The rules of structure control of metallogenic and the rules in enrichment of metallogenesis were studied.
The Qinling Group of Lower Proterozoic is an advantageous environment for metallogenesis and the ductile shear zone is a major structure to control rocks and ores.
The metallogenesis is close related with the Caledonian - Indosinian regional metamorphism.