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南黄海沉积层纵波速度与地震反射特征

吴志强 陆凯

海洋地质与第四纪地质2011,Vol.31Issue(2):73-77,5.
海洋地质与第四纪地质2011,Vol.31Issue(2):73-77,5.DOI:10.3724/SP.J.1140.2011.02073

南黄海沉积层纵波速度与地震反射特征

CHARACTERISTICS OF P-WAVE VELOCITY AND SEISMIC REFLECTION OF THE SEDIMENTARY LAYER IN THE SOUTH YELLOW SEA

吴志强 1陆凯2

作者信息

  • 1. 国土资源部海洋油气资源与环境地质重点实验室,青岛266071
  • 2. 青岛海洋地质研究所,青岛266071
  • 折叠

摘要

Abstract

As a superimposed sedimentary basin, the south Yellow Sea Basin contains well developed clastic deposits of Cenozoic to Mesozoic and marine carbonate sediments of early Mesozoic to Paleozoic with interbedded clastic deposits. Based on the logging data with reference to the related data from the north Jiangsu basin, we summarized in this paper the p-wave velocity characteristics of sedimentary sequence in the south Yellow Sea and calibrated the seismic reflection interfaces and sequences.

关键词

纵波速度/反射层序/南黄海

Key words

south Yellow Sea/ p-wave velocity/ reflection sequence/ characteristic

分类

天文与地球科学

引用本文复制引用

吴志强,陆凯..南黄海沉积层纵波速度与地震反射特征[J].海洋地质与第四纪地质,2011,31(2):73-77,5.

基金项目

"南黄海油气资源普查"项目资助 ()

海洋地质与第四纪地质

OA北大核心CSCDCSTPCD

0256-1492

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