摘要
康苏盆地为一山前断陷盆地处于塔里木地台边缘与天山华力西褶皱系汇集地带。构造单元为塔里木地台西缘与天山褶皱系交汇的铁列克坳陷中的康苏盆地。盆地发育的侏罗系地层康苏组为唯一的含工业煤层段。
Kang su basin is a piedmont fault basin on the verge of tarim platform and tianshan variscan folded system gathering zone. Tectonic units in the tarim platform margin and tianshan fold system of kang su of iron in column g depression basin. Basin of Jurassic stratigraphic kang su group as the only industrial seam.
出处
《世界有色金属》
2016年第4S期79-,81,共2页
World Nonferrous Metals
关键词
康苏盆地
地层构造
沉积特征
Kang su basin
layered structure
sedimentary characteristics
