1.
Advances of Geochemical Behavior of Chalcophile Elements and Applications in Metallogeny of Magmatic Cu-Ni-PGE Sulfide Deposits
亲铜元素的地球化学行为研究进展及其在岩浆硫化物矿床中的应用
2.
Magma Evolution and Sulfide Mineralization of the Karatongk Ni-Cu Sulfide Deposit, Xinjiang, China;
新疆喀拉通克铜镍硫化物矿床成矿岩浆作用
3.
Metallogenic magmatism of Huangshan Cu-Ni sulfide deposit in Xinjiang
新疆黄山铜镍硫化物矿床成矿岩浆作用过程
4.
Geological and Geochemical Characteristics of the Magma Conduit-Type Orebodies of Jinchuan Cu-Ni Sulfide Deposit
金川铜镍硫化物矿床岩浆通道型矿体地质地球化学特征
5.
Petrogenesis of Kalatongke Cu-Ni sulfide deposit in Xinjiang
新疆喀拉通克铜镍硫化物矿床成矿岩浆作用过程
6.
The magma originated from the upper mantle and belongs to the tholeiitic series which has undergone immiscible separation of metal sulfide.
岩浆起源于上地幔,属于拉斑玄武岩系列,发生过金属硫化物的熔离作用。
7.
Metallogenic Process and Exploration of Magmatic-association Metallic Sufide Deposits of Qilian Mountain, Northwest China;
祁连山岩浆作用有关硫化金属矿床成矿与找矿
8.
THE PHYS1COCHEMICAL CONDITIONS OF THE PORPHYRY MAGMATISM IN THE NORTHERN PART OF THE EAST QINLING
东秦岭北部斑岩岩浆作用的物理化学条件
9.
PHYSICOCHEMICAL CONDITION OF MAGMATISM IN YULONG PORPHYRY COPPER BELT, EASTERN TIBET
藏东玉龙斑岩铜矿带岩浆作用的物理化学条件
10.
as of molten material, such as lava.
形容那些已熔化的物质如岩浆等溢出。
11.
Nabil M.Hassan and Samia A.Helmy Department of Chemistry, Faculty of Science, University of Cairo,Giza(Egypt)
埃及蔗渣制溶解浆——用碱性硫化物、亚硫酸盐及硫化物—亚硫酸盐溶液蒸煮
12.
Study on Crosslinking of Unbleached Kraft Pulp Catalyzed by Peroxidase
未漂硫酸盐浆过氧化物酶催化交联的研究
13.
molten rock, steel, lava
熔化的岩石、 钢水、 岩浆.
14.
The massive sulfide contains fragments of barren and mineralized gabbro, and schist.
块状硫化物中含有矿化的和未矿化的辉长岩及片岩碎块。
15.
sulfite cellulose extract
亚硫酸盐纸浆提出物
16.
Magmatic Sulphide Copper Nickel-platinum (PGE) Deposit Types, Distribution and Analysis of Platinum Palladium Occurrence States in Emei Basalt;
岩浆硫化铜镍型铂（铂族）矿床类型、分布与峨嵋玄武岩铂钯赋存状态研究
17.
neutral sulphite semichemical pulp
中性亚硫酸盐半化学浆
18.
As magma rises under the mid-ocean ridge, ferromagnetic minerals in the magma become magnetized in the direction of the geomagnetic field.
当岩浆从中海脊下涌起的时候，岩浆中的磁铁矿物质按地磁场的方向被磁化。