南沙群岛海区北部中生界地震特征分析

doi:10.11978/j.issn.1009-5470.2012.04.011

热带海洋学报 ›› 2012, Vol. 31 ›› Issue (4): 83-89.doi: 10.11978/j.issn.1009-5470.2012.04.011 cstr: 32234.14.j.issn.1009-5470.2012.04.011

南沙群岛海区北部中生界地震特征分析

王彦林¹, 阎贫¹, 郑红波¹, 刘海龄¹, 廖林²

1. 中国科学院边缘海地质重点实验室, 中国科学院南海海洋研究所, 广东广州 510301;
2. 广州海洋地质调查局, 广东广州 510760

收稿日期:2011-08-02 修回日期:2011-09-30 出版日期:2012-10-22 发布日期:2012-10-24
通讯作者: 阎贫。E-mail: yanpin@scsio.ac.cn
作者简介:王彦林(1979—), 男, 甘肃省会宁县人，主要从事海洋地质和地震层析成像研究。E-mail: wenhuiwen@163.com
基金资助:
中国科学院知识创新工程青年人才领域前沿项目(SQ201008)；广东省科技计划项目(2011A080403021)；国家自然科学基金项目(41206039、40876027)；国家海洋局海底科学重点实验室开放基金项目(KLSG1206)；海洋地质保障工程项目(GZH20110205)；广州海洋地质调查局局控科研项目(GZHJK2011004)；国家重点基础研究发展计划(“973”计划)项目(2007CB411706)

Stratigraphic and structural characteristics of the northern margin of Nansha Islands waters in the South China Sea

WANG Yan-lin ¹, YAN Pin ¹, ZHENG Hong-bo¹, LIU Hai-ling¹, LIAO Lin²

1. Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;
2. Guangzhou Marine Geological Survey, Guangzhou 510760, China

Received:2011-08-02 Revised:2011-09-30 Online:2012-10-22 Published:2012-10-24

摘要/Abstract

摘要：

一系列的钻探和拖网取样都表明南沙群岛海区东、南部存在中生代海相沉积。新的国家重点基础研究发展计划地震测线经过南沙群岛海区北部, 调查采用了长排列、高分辩率技术。所获地震剖面显示在披覆沉积和裂谷式充填沉积之下, 还存在大套具有密集反射、倾斜形变和高角度断裂的下构造层。结合南海的构造演化过程以及钻探和拖网取样结果对比, 将上覆构造层划为裂谷期及裂谷后期沉积, 下构造层划为中生代沉积。残留的厚层海相中生界呈北东―西南向条带状相间分布, 反映新生代拉张具有明显的块断特点。根据中生界的地层和变形特点, 进一步推断南沙群岛海区北部位于中生代东亚陆缘弧前盆地的近弧一侧。

关键词: 南沙群岛海区, 下构造层, 中生界, 海相, 断块

Abstract:

It was inferred that there were Mesozoic marine deposits in the Nansha Islands waters through extensive seismic reflection profiles, drilling and dredge sample. A new high resolution 2D seismic survey with long cable was carried out along a NNW-SSE line from the southwestern sub-basins of the South China Sea into the northern part of the Nansha Islands waters area in the South China Sea in 2009. It was shown that there is a great set of infrastructure with dipping and closely spaced reflection with high angle fault below rift and drape sedimentation. Through analysis of the drilling and dredge sample of Mesozoic samples in the Nansha Islands waters area, the sedimentary strata are divided into three structure layers by an angular disconformity, which are post-rift, syn-rift and Mesozoic marine sediments, respectively. The NE to WS trending thick Mesozoic was remained in banding distribution, which indicates that the Cenozoic rift structure is primarily characterized by the occurrence of tectonic block. It is inferred that the northern margin of the Nansha Islands waters is located in the fore-arc basin of the East Asian continental margin, close to the magmatic arc, in the Mesozoic.

Key words: Nansha Islands waters, lower tectonic layer, Mesozoic, marine sediment, tectonic block

中图分类号:

P738.4

王彦林, 阎贫, 郑红波, 刘海龄, 廖林. 南沙群岛海区北部中生界地震特征分析[J]. 热带海洋学报, 2012, 31(4): 83-89.

WANG Yan-lin,YAN Pin,ZHENG Hong-bo, LIU Hai-ling, LIAO Lin. Stratigraphic and structural characteristics of the northern margin of Nansha Islands waters in the South China Sea[J]. Journal of Tropical Oceanography, 2012, 31(4): 83-89.

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南沙群岛海区北部中生界地震特征分析

Stratigraphic and structural characteristics of the northern margin of Nansha Islands waters in the South China Sea

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