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南海笔架南盆地地震反射波特征及地震层序地质时代探讨
引用本文:高红芳,白志琳.南海笔架南盆地地震反射波特征及地震层序地质时代探讨[J].地学前缘,2000,7(3):239-246.
作者姓名:高红芳  白志琳
作者单位:广州海洋地质调查局,第二海洋地质调查大队,广州,510760
基金项目:“我国专属经济区和大陆架勘测”专项!(HY1260311)
摘    要:运用地震地层学方法 ,在笔架南盆地识别出 5个特征明显的反射界面 ,划分了 3个超层序、5个地震层序 ,并探讨各地震层序的地质时代。通过地震相沉积相推测分析 ,认为地震层序E主要发育火山碎屑岩相 ;地震层序D主要发育半深海偏泥相 ;地震层序C主要发育半深海泥岩相 ;地震层序B主要发育半深海—深海泥岩相和浊积偏砂相 ;地震层序A主要发育深海泥岩相、深海三角洲泥岩相和浊积偏砂相

关 键 词:笔架南盆地  超层序  地震层序  地质时代  地震相  沉积相

CHARACTERISTICS OF SEISMIC REFLECTION AND GEOLOGIC AGES OF SEISMIC SEQUENCES OF BIJIA'NAN BASIN,SOUTH CHINA SEA
GAO Hong-fang,BAI Zhi-lin.CHARACTERISTICS OF SEISMIC REFLECTION AND GEOLOGIC AGES OF SEISMIC SEQUENCES OF BIJIA'NAN BASIN,SOUTH CHINA SEA[J].Earth Science Frontiers,2000,7(3):239-246.
Authors:GAO Hong-fang  BAI Zhi-lin
Abstract:From seismic stratigraphy, the authors identify five seismic reflection interfaces and differentiate five seismic sequences and three supersequences. Geologic age of seismic sequences is confined to a certain degree. Seismic facies and sedimentary facies are analyzed. There developed pyroclastic rock in the Late Oligocene in the basin, bathyal mudstone and a little sandstone in the Early Miocene, bathyal mudstone in the Middle Micocene and the Late Miocene, bathyal\|deep sea mudstone and turbidite in the Pliocene, and deep sea mudstone, deltaic mudstone and turbidite in the Quaternary.
Keywords:Bijia nan basin  supersequence  seismic sequence  geologic age  seismic facies-sedimentary facies  
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