| 龙永煤田吕凤矿区构造特征及其演化 |
| |
| 引用本文： | 邱荣生.龙永煤田吕凤矿区构造特征及其演化[J].中国西部科技,2007(15). |
| |
| 作者姓名： | 邱荣生 |
| |
| 作者单位： | 福建省121煤田地质勘探队 福建龙岩 |
| |
| 摘 要： | 本文通过吕凤矿区构造特征分析,探讨了该区构造演化过程,即印支晚期主要形成二条滑覆断层;燕山早期形成吕凤背斜;燕山中晚期形成南北边界正、逆断层及岩浆岩,并且使该区构造复杂化。
|
| 关 键 词： | 构造特征 构造演化 吕凤煤矿区 |
Structural Feafure and Its Evolution of Lufeng Mine in Longyong Coalfield |
| |
| QIU Rong-sheng.Structural Feafure and Its Evolution of Lufeng Mine in Longyong Coalfield[J].Science and Technology of West China,2007(15). |
| |
| Authors: | QIU Rong-sheng |
| |
| Abstract: | The paper is anglysed the mine structural evolution process through the feature of Lufeng area.The Lufeng anticline is major fold, formed a lot of secondary folds later period.Exists three type of decollement fault, reversed fault and little fault.Tectonic evolution is following:decollement faut was formed in latter period of Indo-China. Lufeng anticline in early period of Yanshan; normal fault, reversed fault and magma of mine margin in middle and latter period of Yanshan, and complexed the structure. |
| |
| Keywords: | struitural feature evolution coal mine of Lufeng |
| 本文献已被 CNKI 维普 等数据库收录！ |
|
