摘要
蚣坝、水市地区位于华南褶皱系南岭构造带中段北缘，泥盆纪地层广布测区，南部其昌岭基底隆起导致区内古地理环境的巨大变迁，岩石组合复杂，岩相类型多样，致使区内不同时期、同一时期不同区域的岩相演化特征有着不同的特点。
Gongba and Shui areas, situated at the northern edge in the middle of Nanling tectonic zone, Huanan fold system, with widely distributed Devonian period stratum, huge variance of paleogeographic environment caused by basement uplift of the southern Qichangling, complex rock combination, and lots of lithofacies types, had varied traits of lithofacies evolvement at different period or the same period at varied zones.
出处
《湖南地质》
2002年第3期175-181,共7页
Hunan Geology
关键词
湖南
水市地区
蚣坝地区
泥盆纪
岩相古地理
沉积相
Sedimentary facies
Paleogeography
Qichangling
Devonian period
Gongba
Shuishi region
