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晋北晚古生代煤系高岭岩的特征及成因
引用本文:朱如凯, 孙亚芸, 张运东. 1997. 晋北晚古生代煤系高岭岩的特征及成因. 地质通报, 16(2).
作者姓名:朱如凯  孙亚芸  张运东
作者单位:1. 中国石油天然气总公司北京石油勘探开发科学研究院;; 2. 中国地质科学院尾矿综合利用中心;; 3. 中国地质大学
摘    要:晋北晚古生代煤系中的高岭岩,其主要类型和富集层是:(1)本溪组底部的铝土质高岭岩;(2)太原组夹矸高岭岩;(3)山西组夹矸高岭岩。根据不同层位高岭岩的岩石、矿物、地球化学特征的差异,分析了高岭岩可能的源岩性质,并探讨了其成因和形成的模式

关 键 词:高岭岩   夹矸高岭岩   源岩   成因模式

TYPES, GEOCHEMISTRY AND GENESIS OF KAOLIN ROCK IN NORTHERN SHANXI
1997. TYPES, GEOCHEMISTRY AND GENESIS OF KAOLIN ROCK IN NORTHERN SHANXI. Geological Bulletin of China, 16(2).
Authors:Zhu Rukai
Affiliation:1. Beijing Research Institute of Petroleum Exploration and Development, Beijing;; 2. Chinese Academy of Geological Sciences, Beijing;; 3. China University of Geoscience, Beijing
Abstract:The authors studied the petrology, mineralogy and geochemistry of kaolin rock in Late Paleozoic coal measures in northern Shanxi. The major types and accomudation horizons are: ① bauxitic kaolin rock at the base of the Benxi Formation, ② tonsteins in the Taiyuan Formation, and ③ tonsteins in the Shanxi Formation. The differences in petrology, mineralogy and geochemistry of different horizons are related to the genesis and source rocks of the rock.
Keywords:kaolin rock   tonstein   source rock   genesis  
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