摘要
根据楚雄盆地边缘露头分布与盆地内地震勘探成果来预测盆地内不同相带地层的分布。本文对楚雄盆地晚三叠世海相沉积展布进行探讨,认为该层在反射地震剖面上有明显的特征显示,可以确定它的平面展布。
Based on the strata distribution of Chuxiong basin margin and the results of seismic 'prospecting in the basin, the distribution of strata of various facies can be predicated. In this paper, the distribution of Late Triassic marine sedi-ments in Chuxiong basin is discussed. It is conserdered that the plan distribu-tion of this stratum can be determined by the obvious feature of seismic ref-lection section.
出处
《云南地质》
1992年第1期21-23,共3页
Yunnan Geology
