| 甘肃公婆泉铜矿区斑岩岩浆起源及成岩成矿大地构造背景 |
| |
| 引用本文： | 游小毛.甘肃公婆泉铜矿区斑岩岩浆起源及成岩成矿大地构造背景[J].大地构造与成矿学,1999,23(2):167-171. |
| |
| 作者姓名： | 游小毛 |
| |
| 作者单位： | 中南工业大学地质系,长沙,410083 |
| |
| 摘 要： | 探讨了公婆泉矿区斑岩岩浆起源，论述了该矿区斑岩成岩成矿大地构造背景。研究结果表明，该矿区斑岩岩浆起源属幔壳混合源；斑岩成岩成矿大地构造背景为褶皱造山期。
|
| 关 键 词： | 成岩成矿大地构造背景 岩浆起源 斑岩 公婆泉铜矿床 甘肃北山 |
RESEARCH ON MAGMA ORIGIN AND MINEROGENETIC GEOTECTONIC BACKGROUND OF PORPHYRY IN GONGPOQUAN COPPER ORE DISTRICT, GANSU PROVINCE |
| |
| YOU Xiaomao.RESEARCH ON MAGMA ORIGIN AND MINEROGENETIC GEOTECTONIC BACKGROUND OF PORPHYRY IN GONGPOQUAN COPPER ORE DISTRICT, GANSU PROVINCE[J].Geotectonica et Metallogenia,1999,23(2):167-171. |
| |
| Authors: | YOU Xiaomao |
| |
| Abstract: | This paper researches into magma origin and minerogenetic geotectonic background of porphyry in the Gonpoquan copper ore district. The results show that the porphyry magma was mantle crust mixed type magma and the minerogenetic geotectonic background of porphyrpy was orogenic phase. |
| |
| Keywords: | Minerogenetic geotectonic background magma origin porphyry Gongpoquan copper deposit Beishan region Gansu |
| 本文献已被 维普 万方数据 等数据库收录！ |
