首页 | 本学科首页   官方微博 | 高级检索  
     检索      

铁法盆地同沉积构造与聚煤
引用本文:吴志国,王宇林.铁法盆地同沉积构造与聚煤[J].黑龙江科技学院学报,2007,17(3):185-189.
作者姓名:吴志国  王宇林
作者单位:1. 辽宁省地勘局第十地质大队,辽宁,抚顺,113007
2. 辽宁工程技术大学,资源与环境工程学院,辽宁,阜新,123000
基金项目:国家重点基础研究发展计划(973计划)
摘    要:铁法盆地属于晚中生代的NNE向半地堑煤盆地,北西西系是其主要的成盆期构造.在对铁法盆地的同沉积构造进行重新认识的基础上,划分了纵向同沉积构造单元和横向同沉积构造单元,分析了各同沉积构造单元的聚煤条件、控煤特点,总结出其对富煤带和聚煤中心的控制作用,确定了中部较缓慢沉降带、东部缓慢沉降带中近岸浅水湖泊区及湖缘三角洲平原为远景找煤方向.

关 键 词:同沉积构造  冮屯断裂  聚煤  铁法盆地  铁法盆地  同沉积构造  聚煤  basin  accumulation  coal  找煤方向  三角洲平原  湖缘  浅水湖泊  东部  沉降  控制作用  中心  富煤带  控煤  条件  分析  构造单元  划分
文章编号:1671-0118(2007)03-0185-05
修稿时间:2007-03-24

Syndepositional structure and coal accumulation in Tiefa basin
WU Zhiguo,WANG Yulin.Syndepositional structure and coal accumulation in Tiefa basin[J].Journal of Heilongjiang Institute of Science and Technology,2007,17(3):185-189.
Authors:WU Zhiguo  WANG Yulin
Institution:1. No. 10 Geological Team of Liaoning Bureau of Geology and Mineral Resources, Fushun 113007, China; 2. College of Resource and Environment Engineering of Liaoning Technical University, Fuxin 123000, China
Abstract:Tiefa basin is a late Mesozoic NNE-trending half gTaben coal-bearing basin, and the NWW structural system is the most important synbasinal structure. Based on analyzing syndepositional structure of Tiefa basin, the vertical and transversal syndepositional tectonic-units were set out and the coal-controlling characteristic and coal-accumulating condition of syndepositional tectonic-units were analyzed and the control action of synbasinal structure acting on coal-rich zone and coal-accumulating contre was summed up. At last, the aspect and prospect area of coal is the shallow alongshore lake country and lake brim delta plain in the center and eastern slow depression area.
Keywords:syndepositional structure  Gangtun fault  coal accumulation  Tiefa basin
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号