摘要
根据野外考察和有关分析资料,阐述了昆明盆地的泥炭赋存特征及其成因,並对聚煤环境进行了类比分析。从成炭机理的类同性大致反映出古地理演变的基本过程,亦为寻找和勘探泥炭与褐煤资源提供了一定的科学依据。
There are rich resources of peat in Kunming Basin. They are main distributed in the delta of pan long river in the northern bank of Dian Chi lake. The peat distribution character is determined of conditions which are geology, geomorphology and hydrology. The peat has been formed chiefly since Holocene. The climatic condition is advantageous to the peat bog formation and development since Quaternary. The peat and coal environment of formation are concerned directly and indirectly with agent of longitudinal rivers.
出处
《南京师大学报（自然科学版）》
CAS
CSCD
1989年第4期90-96,共7页
Journal of Nanjing Normal University(Natural Science Edition)
关键词
昆明盆地
泥炭
褐煤
聚煤环境
Kunming Basin, peat distribution charaeter, peat and coal environment of formation.
