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万安盆地构造沉降与沉积速率及其油气资源前景
引用本文:施秋华,夏斌,万志峰,张云帆.万安盆地构造沉降与沉积速率及其油气资源前景[J].沉积与特提斯地质,2014(2):43-46.
作者姓名:施秋华  夏斌  万志峰  张云帆
作者单位:[1]中国科学院广州地球化学研究所,广东广州510640; [2]中山大学海洋学院,广东广州510275; [3]中国科学院南海海洋研究所,广东广州510301
基金项目:中国科学院边缘海地质重点实验室课题(MSGL11-03); 国家重点基础研究发展计划(973)(2009CB219401)联合资助
摘    要:万安盆地是南海重要的新生代含油气盆地之一,是较为典型的新生代走滑拉张盆地。根据对横穿盆地的地震反射剖面的平衡剖面模拟和构造沉降速率、沉积速率的计算,认为万安盆地曾经历了3次快速的构造沉降。2.6Ma以来,沉积速率最大。万安盆地的沉降与沉积速率和盆地构造演化过程密切相关,各构造演化阶段分别控制了盆地中油气的生成、运聚和保存等成藏条件与过程。

关 键 词:构造沉降  构造演化  沉积速率  万安盆地
收稿时间:2013/5/30 0:00:00
修稿时间:2013/9/8 0:00:00

Tectonic subsidence, sedimentary rates and petroleum resources potential in the Wan'an Basin
SHI Qiu-hu,XIA Bin,WAN Zhi-feng,ZHANG Yun-fan.Tectonic subsidence, sedimentary rates and petroleum resources potential in the Wan'an Basin[J].Sedimentary Geology and Tethyan Geology,2014(2):43-46.
Authors:SHI Qiu-hu  XIA Bin  WAN Zhi-feng  ZHANG Yun-fan
Affiliation:SHI Qiu-hua,XIA Bin,WAN Zhi-feng,ZHANG Yun-fan(1. Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, Guangdong, China; 2. School of Marine Sciences, Sun Yat-Sen University, Guangzhou 510275, Guangdong, China; 3. South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, Guangdong, China)
Abstract:The Wan'an Basin as one of major Cenozoic petroleum basins in the South China Sea is a representative Cenozoic strike-slip pull-apart basin.Inferred from the calculations of balanced profile modeling,tectonic subsidence rates and sedimentary rates for the basinwide seismic reflection profiles,the Wan'an Basin may have experienced three phases of rapid tectonic subsidence.The sedimentary rates also came up to a climax from the 2.6Ma onwards.A close correlation exists between the tectonic subsidence rates and sedimentary rates of the basin,which have exercised a major control on the generation,accumulation,migration and preservation of the hydrocarbons in the basin.
Keywords:tectonic subsidence  tectonic evolution  sedimentary rate  Wan'an Basin
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