1.Similarly, high heat flows are to be expected among the active or not-too-long extinct magmatic belts of plate approximation zones.
同样，在板块相互靠近的地带的活动岩浆带或熄灭不久的岩浆带中也可以出现高热流。
2.Between them, main and trace elements display the magmatic mixing evolution trend.
二者在主量和微量元素上表现出岩浆混合成因的演化趋势。
3.Magmatic PGE sulfide deposit in melanocratic rock series is still one of the fundamental sources of PGE resources.
暗色岩套中的硫化物PGE矿床仍然是目前PGE资源的主要来源之一。
4.Widespread magmatic rocks, the area from the east to the Himalayan period since the intensity of the magma activity times.
区域普遍分布的岩浆岩，是从加里东期至喜马拉雅期以来分歧强度的多期次岩浆勾当的产物。
5.Metallogenic fluids are mainly rock formation water and meteoric water as well as possible addition of magmatic hydrothermal solutions.
矿床成矿流体以建造水和大气降水为主，并可能有岩浆热液的加入。
6.The most efficient ore components concentration mechanism at the magmatic stage must be the separation of fluid melt.
在岩浆阶段，富集金属元素最有效的机制是流体熔体的分离。
7.Kalatongke Cu Ni deposit is of magmatic seperation type ore deposit occurring in orogenic belt far from craton.
喀拉通克铜镍矿床为产出于造山带且远离克拉通的岩浆熔离型铜镍矿。
8.Neoproterozoic magmatic rocks, especially granitic intrusions, are widespread in the western margin of the Yangtze craton.
扬子地块西缘新元古代岩浆活动非常强烈，花岗岩广布。
9.Ore bering fluid was orignated from magmatic water for the early period and with ihtro-duction of strata water for the late.
含矿流体来源早期以岩浆为主，晚期有地层水的加入。
10.The deposit was produced by superimposition of the hot-water sedimentary mineralization and magmatic hydatogenesis.
该矿床是热水沉积成矿作用与岩浆热液成矿作用叠加成矿的产物。