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西沙海域新近纪生物礁的发育演化及控制因素

杨振 张光学 张莉 夏斌

石油实验地质2016,Vol.38Issue(6):787-795,9.
石油实验地质2016,Vol.38Issue(6):787-795,9.DOI:10.11781/sysydz201606787

西沙海域新近纪生物礁的发育演化及控制因素

Development and controlling factors of Neogene reefs in Xisha sea area

杨振 1张光学 1张莉 1夏斌2

作者信息

  • 1. 国土资源部 海底矿产资源重点实验室,广州海洋地质调查局,广州 510075
  • 2. 中山大学 海洋学院,广州 519082
  • 折叠

摘要

Abstract

During the Neogene a large number of reefs developed in the Xisha sea area with a great potential for oil and gas exploration. High⁃resolution seismic data and extensive well drilling data provided an opportunity to under⁃stand the evolution of reefs in this area. A few reefs initially developed on a basement high in the early Miocene. In the early Middle Miocene, the reefs, such as point reefs, platform⁃edge reefs, and pinnacle reefs, flourished on the western slope of Xisha Uplift. They gradually back stepped to the elevated topographic highs in response to a relative sea level rise. In the late Middle Miocene, reefs began to wither and mainly grew on the Xisha Uplift represented by horse toe reefs and platform⁃edge reefs. Since the Late Miocene, many reefs formerly developing on the edge of the Xisha Uplift were submerged and only some atolls survived around the islands on the Xisha Uplift. Tectonics and eustasy controlled the development of Neogene reefs in the Xisha sea area. Tectonics controlled the topography for the initial growth of reefs, and tectonic subsidence combined with rapid relative sea⁃level changes controlled reef evolution during the Neogene. In addition, the rhythm of relative sea⁃level changes in a short time also influenced the sedimen⁃tary cycles of reefs.

关键词

生物礁/发育模式/控制因素/新近纪/西沙海域

Key words

reef/evolutionary model/controlling factors/Neogene/Xisha sea area

分类

能源科技

引用本文复制引用

杨振,张光学,张莉,夏斌..西沙海域新近纪生物礁的发育演化及控制因素[J].石油实验地质,2016,38(6):787-795,9.

基金项目

中国地质调查局项目(GZH20120511)和国家基金委南海重大计划-重点基金项目(91228208)资助。 ()

石油实验地质

OA北大核心CSCDCSTPCD

1001-6112

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