前 言 本文拟探讨南海北部沿岸最近6,000年来的海面变动与近代地壳运动. 众所周知,全新世的海面变动,其中包括近6,000年来是否有高海面问题,曾引起广泛的争论.总的说来,大致有R.W.费尔布里奇和F.P.谢帕德两种有代表性的观点.前者认为大西洋期的海面比今天海面高出3—6米,并从那时起,海面具有多次的波动;后者认为全新世既没有高海面,也非波动的. Preface This paper is intended to explore the recent 6,000 years of sea surface movement and the recent crustal movement in the northern coast of the South China Sea. It is known that the Holocene sea-level changes, including the high sea level in the past 6,000 years, have caused widespread controversy. RW Felbridge and FP Shepard, the former arguing that the Atlantic Ocean is 3-6 meters above sea level today and that there has been a number of sea-level fluctuations since then Holocene that neither the sea nor the volatility.