晋北晚古生代煤系高岭岩的特征及成因

详细信息

TYPES, GEOCHEMISTRY AND GENESIS OF KAOLIN ROCK IN NORTHERN SHANXI

1. Beijing Research Institute of Petroleum Exploration and Development, Beijing;
2. Chinese Academy of Geological Sciences, Beijing;
3. China University of Geoscience, Beijing

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
- 高岭岩 /
- 夹矸高岭岩 /
- 源岩 /
- 成因模式
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.
- kaolin rock /
- tonstein /
- source rock /
- genesis