昆明地区近期地面垂直升降运动及分析
Recent up-and-down ground motion in Kunming area and its analysis
区内以造陆性垂直升降运动为主,除奥陶系与志留系整合接触外,其余为平行不整合接触。
Except the conformable contact between the Ordovician and Silurian , the other contact layers are marked by parallel unconformities .