摘要
广东新构造运动区划：Ⅰ广东大地块区，Ⅱ雷州半岛区。Ⅰ区再分为：Ⅰ_１大河河源亚区，Ⅰ_２广东地块亚区，Ⅰ_３潮汕平原亚区。该区划的部分分界位置湛江和灯塔，与海岸线基本走向的转折点较一致，多数ＮＥ向断裂自晚更新世以来其造貌运动的差异性不明显。
The divisons of Guangdong province on new structure motion are:I Guangdonggreat massif area, Ⅱ Leizhou Peninsula area ; the Ⅰarea is further divided into:_1 second areaof big river head,I_2 second area of Guangdong massif,I_3 second area of Chaoshan Plain。Some places in the dividing lines,e.g. Zhanjiang, Dengta, and the turning points of basic trendsof coastline, are identical.The differences of building landform motion by most NE faults havenot been clear since Pleistocene Epoch。
出处
《中山大学学报（自然科学版）》
CAS
CSCD
1995年第4期93-99,共7页
Acta Scientiarum Naturalium Universitatis Sunyatseni
关键词
广东
新构造运动
海岸线
发育
Guangdong,new structure motion,coastline,Leizhou Peninsula, Pearl RiverDelta,Chaoshan Plain
