摘要
本文系统地讨论了长兴期层序地层特征，确定了长兴期沉积层的顶、底界线。以单因素图件为基础，结合其它成因标志，编制了长兴期岩相古地理图，由此可以看出皖南地区长兴期的岩相古地理展布规律。
Based on the discussion of characteristics of the sequence stratigraphy,the upper and lower boundaries of changxing Age sedimentary formation are detemined.The lithofacies paleogeographic map in changxing Age is worked out on the basis of the single factor maps combined with other genesis indexes,then the diotribution characteristics of lithofacies paleography of changxing Age can be seen.
出处
《山东矿业学院学报》
CAS
1996年第3期5-8,共4页
Journal of Shandong University of Science and Technology(Natural Science)
