摘要
位于我国东南沿海的福建省,东濒台湾海峡,与祖国宝岛台湾省隔海相望,海岸线漫长曲折。前人对我省海岸升降做了很多工作。德国人李希霍芬1912年提出中国海岸以杭州湾为界,杭州湾以北是上升的,以南是下降的。林观得认为福建海岸是上升的。还有许多人认为华南海岸以上升为主,有升有降。作者经过多年的野外调查,结合前人的资料,认为我省海岸大致以福清龙江为界,龙江以北的福鼎—长乐海岸,以下降为主。龙江以南的福消—诏安海岸,以上升为主,但也发生过较大幅度的下降;局部地段则以下降为主。
Various marks of coastal rise and fall of Fujian Province are listed in this paper and we hold that the Fuding—Changle Coast,north of Longjiang,Fuqing is mainly of falling coast and the Fuqing—Shaoan Coast,south of Longjiang is mainly of rising coast where great amplitude of falling also happened in the past.Some problems of morphological Quaternary geology related to the rise and fall of the coast are discussed.Based on the development law of Quaternary strata,we believe that Fujian coast has seen rise—relative stabilization—great fall—small rise since Quaternary.On studying the general morphology,that the morphological landscape of Fujian Coast is of falling coast is concluded.
作者
陈园田
Chen Yuantian(Comprehensive Survey Group,Fujian Provincial Bureau of Seismology)
出处
《台湾海峡》
CAS
1982年第1期62-68,共7页
Journal of Oceanography In Taiwan Strait
