下元古界秦岭群是成矿有利环境，韧性剪切带是控岩控矿的主要构造。
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.
这一特殊构造环境，对铀成矿有利。
This specific structural environment is favourable for uranium mineralization.
本文阐述了该火山洼地形成的历史背景、大地构造环境、形成时地壳运动的特点及与成矿作用的关系。
This paper elucidates the historical setting, the geotecto- hie environment, the features of the crustal movement and their relation to mineralization during the formation of the volcano—tectonic.
裂谷及微型裂陷等拉张性构造环境有利于深部岩浆与成矿物质的上升。
The tension tectonic environment like rift and micro-aulacogen are favourable for up-welling of underground magma and metallogenic elements.
但在矿床与构造环境、构造与成矿物理化学条件及成因模型等方面还有待于深入研究。
In some respects, such as relations between deposit and tectonic setting, mineralization physical chemical condition and structure, and genetic model and so on, many questions are waiting.
随着变形机制、构造环境变化引起成矿流体沸腾作用并导致金矿形成。
With the change of strain dynamic and tectonic situation, ore fluids boil and result the formation of gold deposit.
北祁连金属成矿省在地质历史演化过程的不同构造环境内形成了四个主要金属成矿幕。
Four metallogenetic epochs occurred in different tectonic environments during the evolution of the Northern Qilian metallogenetic province through geological time.
西昆仑以其强烈的构造变形、频繁的岩浆活动、漫长的地质演化历史及特殊的大地构造环境而具有得天独厚的成矿地质条件。
Magmation was frequent, tectonic deformation was violent, the history of geological evolvement was long and geological condition of producing mineral was good in West Kunlun.
火山构造成岩-成矿作用过程中，体系与其环境之间的能量与物质交换，发生各种非线性的不可逆过程。
In the course of rock formation and mineralization of volcanic structure, exchange of energy and material between the system and its environment occurs as various non-linear irreversible processes.
从区域成矿地质背景及控矿因素来看，大地构造环境制约着“矿源层”及赋矿地层的形成，区域断裂构造控制着金成矿带及金矿床的空间分布。
The formation and distribution of gold-deposits were controlled by tectonic setting in the area. The gold deposits controlled by ore-forming structure were discussed in this paper.
本文对鄂尔多斯盆地和塔里木盆地铀矿床(含矿化集中区)进行了遥感研究，发现其成矿环境与断块隆起(断隆构造)密切相关。
Through remote sensing research of uranium deposit in Ordos and Tarim basins, the close relationship of its metallogenic environment and fault-block uplift (fault-uplift structure) was found.
马厂箐铜钼金矿床是“三江”成矿带上与喜马拉雅期富碱斑岩有关的典型矿床之一，产于印支板块与扬子板块碰撞构造环境。
Cu-Mo-Au deposits in Machangqin are typical ores relevant to alkali-rich porphyries of Himalayan movement in"Sanjiang"metallogenic belt, locating at collision environment of Yangtz and Indian plates.
马厂箐铜钼金矿床是“三江”成矿带上与喜马拉雅期富碱斑岩有关的典型矿床之一，产于印支板块与扬子板块碰撞构造环境。
Cu-Mo-Au deposits in Machangqin are typical ores relevant to alkali-rich porphyries of Himalayan movement in"Sanjiang"metallogenic belt, locating at collision environment of Yangtz and Indian plates.
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