摘要
凯里虎庄背斜具有独特的构造特征 :即①在剖面上的不均匀性 ,从地表向下具有不同的构造层次 ,它们属于不同构造期的产物。②由于北东向的鱼洞—樟木树断层为晚古生代的同沉积断层 ,控制了断层两盘志留系的剥蚀和泥盆系的沉积 ,并使两盘构造产生了明显的差异。
Huzhuang anticline,Kaili,Southeast Guizhou,has distinctive structural characteristics:(1)The uneven distribution in longitudinal section indicates various tectonic levels from the earth's surface downwards.(2)The Yudong Zhangmushu fault in northeast direction is a growth fault formed in late palaeozoic era,controlling the denudation in Silurian and the deposition in Devonian at the plates of the fault and making the structure at the two plates remarkably different.The authors' studies suggest that this distinctive structure provides a favourable environment for the preservation of oil and gas.
出处
《贵州工业大学学报（自然科学版）》
CAS
2001年第1期20-23,共4页
Journal of Guizhou University of Technology(Natural Science Edition)
基金
滇黔桂石油勘探局资助!项目<滇黔桂碳酸盐岩地区最佳油气保存单元的选择与评价>的子课题<黔南及南盘江地区构造保存条件研究>的部分成
