| 贵州织金煤矿区龙潭组岩石特征及其意义 |
| |
| 引用本文： | 陶述平,谭西德,等.贵州织金煤矿区龙潭组岩石特征及其意义[J].湖南地质,2001,20(4):247-249,255. |
| |
| 作者姓名： | 陶述平 谭西德 |
| |
| 作者单位： | 湘潭工学院 湖南湘潭411201
(陶述平，谭西德)，湘潭工学院 湖南湘潭411201(黄昔容) |
| |
| 摘 要： | 织金矿区含煤地层为上二叠统龙潭组，含主要可采煤6层。煤系地层以含玄武岩屑、海绿石为特征的5类碎屑岩夹碳酸盐岩，水平、沙纹、波状层理发育，煤系中稳定的灰岩、硅铁质灰岩标志层较多，有利于煤层的划分与对比，并产丰富的动植物化石及碎块。属海、陆交替环境下的标型海陆交互相沉积。
|
| 关 键 词： | 龙潭组 海陆交互期 岩石学特征 煤层对比 |
ROCK CHARACTERISTICS OF LONGTAN FORMATIONOF ZHIJIN COAL-MINE IN GUIZHOU AND ITS SIGNIFICANCE |
| |
| TAO,Shu-pingTAN Xi-deHUANG,Xi-rong.ROCK CHARACTERISTICS OF LONGTAN FORMATIONOF ZHIJIN COAL-MINE IN GUIZHOU AND ITS SIGNIFICANCE[J].Hunan Geology,2001,20(4):247-249,255. |
| |
| Authors: | TAO Shu-pingTAN Xi-deHUANG Xi-rong |
| |
| Abstract: | Stratum containing coal of Longtan Formation in Zhijin mine zone include mainly 6 layers of coal that can be picked. In coal beds, five sorts of clasolite with the characteristics of basalt bits and glauconite mixed with carbonate, bedding development of horizon, sand-vein, wave-shape, and lots of key beds of steady (silicon-iron) limestone, favour division and comparison. Plentiful zoolite and phytolite and fragment occur also in the coal bed. This bed belongs to typomorphic paralic deposition under paralic circumstance. |
| |
| Keywords: | Zhijin mining area Rock characteristics Longtan Formation |
| 本文献已被 CNKI 维普 等数据库收录！ |
|
