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721两铀矿床的花岗斑岩体特征
引用本文:薛振华. 721两铀矿床的花岗斑岩体特征[J]. 华东地质学院学报, 1993, 16(1): 7-15
作者姓名:薛振华
作者单位:华东地质学院地质系
摘    要:

关 键 词:铀矿床 花岗斑岩 岩体 控矿构造

GRANITIC-BODY FEATURES OF 721 TWO URANIUM MINERAL DEPOSITS
Xue Zhenghua. GRANITIC-BODY FEATURES OF 721 TWO URANIUM MINERAL DEPOSITS[J]. Journal of East China Institute of Technology, 1993, 16(1): 7-15
Authors:Xue Zhenghua
Affiliation:Department of Geology
Abstract:The two uranium mineral-deposits of 721-2 and 721-18 in northern part of Xianshan uranium mineral deposits are 1.5 km far from each other. The mineral-bodies of the two mineral deposits are mainly existed in the contacting zone of granite-porphyry and adjoining rock. The two small rock-masses of granite-porphyries formed in Yanshan period are formed through anatexis of base shallow metamorphic-rock of Sinian System. The two small rock-masses of the same source intrude upward along the intersection parts of base fissure when the granite-porphyry develope structure coincided and threaded together with the base high angle, endowed uranium ore-bodies develope in it through strong sodium metasomatism.
Keywords:Granite-porphyry  pay structure  fracture  sodium metasomatism
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