摘要
对阿其克库都克盆地下二叠统成煤地质条件、古气候、古环境及含煤性、煤质特征和远景预测,进行了实地调查和分析研究.经孢粉鉴定和煤质分析,该区煤系地层时代为早二叠世,煤的变质程度已达焦煤阶段.下二叠统煤系地层的发现,在天山地区尚属首次,可作为一个新的成煤时期引起重视.
At the south edge of Aqqikkuduk Basin, a coal-series strata cropping out about 2km2 has been discoved. There are four minable coal beds in it with average thickness of about 15m. The sporo-pollen analysis indicates that the coal-series strata are of early Permian. The coal content analysis shows that the metamorp-hism reaches the coking coal stage. From analysis of coal-forming condition and later reformation, it is believed that Aqqikkuduk Basin has a bright future in looking for coking coal.
出处
《新疆地质》
CAS
CSCD
1991年第4期323-328,共6页
Xinjiang Geology
关键词
阿其克库都克
盆地
早二叠世
古地理
焦煤阶段
Xinjiang, Aqqikkuduk Basin, early Permian, palacogeographic enviroment, coking coal stage