摘要
台湾地区第四纪地层分布广泛，沉积厚度大，成因类型复杂。它划分为早更新世—中更新世早期头科山组、中更新世中期大南湾组、中更新世晚期—晚更新世冲—洪积层、晚更新世中—晚期恒春石灰岩层、全新世冲积层和全新世珊瑚礁。上述各地层单位基本上可与福建省的镇海组（Q1）、同安组（Q2）、龙海组（Q3）、长乐组（Q4）进行对比。
The Quaternary strata are wide-spread in Taiwan Region with varied sedimentary depth and complicate genetic types. It can be subdivided into Toukeshan Formation of Early to Middle Pleistocene,Dananwan Formation of middle stage of Middle Pleistocene,AJluvial-pluvial Layer of late stage of Middle Pleistocene to Late Pleistocene,Hengchun Lime8tone Layer of middle to late stage of Late Pleistocene,Holocene Alluvial Layer and Holocene Coral Reef.The stratigraphic units above-mentioned can be correlated basically with Zhenhai Formation (Q1),Tongan Formation (Q2),Longhai Formation (Q3)and Changle Formation (Q4) in Fujian area.
出处
《台湾海峡》
CAS
CSCD
1996年第3期235-242,共8页
Journal of Oceanography In Taiwan Strait
关键词
第四纪地层
时代划分与对比
台湾地区
Quaternary strata, chronological division and correlation, Taiwan
