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西秦岭中川花岗岩岩浆活动特征及地质效应
引用本文:卢哲,权君娟,程彧,闫德飞. 西秦岭中川花岗岩岩浆活动特征及地质效应[J]. 甘肃地质, 2003, 12(2): 25-30
作者姓名:卢哲  权君娟  程彧  闫德飞
作者单位:[1]甘肃省有色金属地质勘查局天水总队,甘肃天水741020 [2]西北有色金属地质勘查局717队,陕西宝鸡721004 [3]甘肃省有色金属地质勘查局,甘肃兰州730000 [4]兰州大学资源环境学院,甘肃兰州730000
摘    要:西秦岭中川花岗岩为3期5次侵入的复式岩体,其主侵入体为印支—燕山期黑云母同碰撞S型二长花岗岩。该岩浆活动在沉积建造中形成热变质作用带和岩浆侵位构造,并产生成矿地质效应。

关 键 词:中川花岗岩  复式岩体  岩浆活动  地质效应

CHARACTERISTICS AND GEOLOGICAL EFFECTS OF MAGMATIC ACTIVITYOF THE ZHONGCHUAN GRANITE OF WESTERN QINLING AREA
LU Zhe,QUAN Jun-juan,CHENG Yu and YAN De-fe. CHARACTERISTICS AND GEOLOGICAL EFFECTS OF MAGMATIC ACTIVITYOF THE ZHONGCHUAN GRANITE OF WESTERN QINLING AREA[J]. Acta Geologica Gansu, 2003, 12(2): 25-30
Authors:LU Zhe  QUAN Jun-juan  CHENG Yu  YAN De-fe
Affiliation:LU Zhe1,QUAN Jun juan4,CHENG Yu2,3,YAN De fei3(1Tianshui Team,Gansu Provincial Bureau of Geology and Exploration for Non ferrous Metals,Tianshui 741020,China;2Gansu Provincial Bureau of Geology and Exploration for Non ferrous Metals,Lanzhou 730000,China;3Resources and Environmental College,Lanzhou University,Lanzhou 730000,China;4No.717 Team,Northwest Bureau of Geology and Exploration for Non ferrous Metals,Baoji 721004,China)
Abstract:Zhongchuan granite of western Qinling area is a granite complex.Its principal in-trusion is Indo-yanshanian S-type biotite adamellite.Magmatic activity led to the formation ofthermo metamorphism belts and to the magmatic intrusive structures and at the same time pro-duced geological effects.
Keywords:Zhongchuan granite  Granite complex  Magmatic activity  Geological effects
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