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河北承德若干矿床成矿流体特性及对矿化类型的制约
引用本文:徐启东,刘承山.河北承德若干矿床成矿流体特性及对矿化类型的制约[J].现代地质,1993,7(2):205-214,T001.
作者姓名:徐启东  刘承山
作者单位:中国地质大学,中国地质大学,河北地质四队,河北地质五队 武汉,武汉
摘    要:小寺沟、轿顶山矿化是由中等盐度的流体侵位于浅部脆性岩石、通过较为迅速的沉淀机制形成的,指示轿顶山具有寻找类似小寺沟斑岩型矿床的潜力;寿王坟矿床的形成与低盐度的流体侵位于深度较大、韧性程度较高的围岩中,与较长时间的渗透交代作用方式有关,不具备形成斑岩型矿床的某些必要条件。研究结果为有关矿区成矿预测提供了矿床成因学方面的论据。

关 键 词:流体包裹体  中等盐度流体  斑岩型矿床  水致裂隙  河北省

CHARACTERISTICS OF ORE-FORMING FLUIDS OF SEVERAL ORE DEPOSITS FROM CHENGDE, HEBEI PROVINCE AND THEIR CONSTRAINTS ON MINERALIZAION TYPE
Xu Qidong Zhu Zhongyi.CHARACTERISTICS OF ORE-FORMING FLUIDS OF SEVERAL ORE DEPOSITS FROM CHENGDE, HEBEI PROVINCE AND THEIR CONSTRAINTS ON MINERALIZAION TYPE[J].Geoscience——Journal of Graduate School,China University of Geosciences,1993,7(2):205-214,T001.
Authors:Xu Qidong Zhu Zhongyi
Institution:Xu Qidong Zhu Zhongyi (China University of Geosciences Wuhan) Liu Chengshan Han Xiude (The Fourth and Fifht Teams of Hebei Bureau of Geology and Mineral Resources)
Abstract:This contrast study reports the investigation of fluid inclusions of three ore deposits from Shouwangfen-Xiaosigou region. These results together with other features of ore geology reveal that Xiaosigou and Jiaodingshan mineralization were formed by the medium- salt-content fluids which entered the brittle rocks in the shallow level by way of a quick- depositing mechanism, which indicates that there is a potential area in Jiaodingshan where a deposit like Xiaosigou Cu-Mo deposit of porphyry may be discovered. But Shouwangfen mineralization was formed by low-salt-content fluid which entered the ductile rocks in the deep level by way of a long-time permeation and replacement mechanism, which does not possess those conditions that are necessary to form the porphyry type deposit. The under- standing of fluid characteristics and their geological meaning may provide the evidence of ore-forming genesis for metallogenic prognosis of the studied ore field.
Keywords:fluid inclusion  medium-salt-content fluid  porphyry trpe deposit  hy-draulic fracture  Hebei Province
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