BIT指标对神狐海域SH7B站位水合物赋存层段生源输入判识及意义

熊萍, 付少英, 江林香, 卢鸿. BIT指标对神狐海域SH7B站位水合物赋存层段生源输入判识及意义[J]. 海洋地质与第四纪地质, 2015, 35(1): 129-134. doi: 10.3724/SP.J.1140.2015.01129
引用本文: 熊萍, 付少英, 江林香, 卢鸿. BIT指标对神狐海域SH7B站位水合物赋存层段生源输入判识及意义[J]. 海洋地质与第四纪地质, 2015, 35(1): 129-134. doi: 10.3724/SP.J.1140.2015.01129
XIONG Ping, FU Shaoying, JIANG Linxiang, LU Hong. BIT INDEX FOR SOURCE AND INPUT IDENTIFICATION OF THE GAS-HYDRATE LAYER AT SH7B STATION IN SHENHU AREA, SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2015, 35(1): 129-134. doi: 10.3724/SP.J.1140.2015.01129
Citation: XIONG Ping, FU Shaoying, JIANG Linxiang, LU Hong. BIT INDEX FOR SOURCE AND INPUT IDENTIFICATION OF THE GAS-HYDRATE LAYER AT SH7B STATION IN SHENHU AREA, SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2015, 35(1): 129-134. doi: 10.3724/SP.J.1140.2015.01129

BIT指标对神狐海域SH7B站位水合物赋存层段生源输入判识及意义

  • 基金项目:

    南海天然气水合物成矿理论及分布预测研究项目(GZH2011003-05-04)、国家科技重大专项(2011ZX05008-002-33)

    国家自然科学基金项目(41173053)。

详细信息
    作者简介: 熊萍(1988-),女,硕士研究生。从事石油地质研究,E-mail:xiongping1988@163.com
  • 中图分类号: P744.4

BIT INDEX FOR SOURCE AND INPUT IDENTIFICATION OF THE GAS-HYDRATE LAYER AT SH7B STATION IN SHENHU AREA, SOUTH CHINA SEA

  • 实际的天然气水合物明显不同于冷泉碳酸盐岩样品。南海已有诸多冷泉碳酸盐岩的研究,针对具有水合物实际产出的神狐海域沉积物样品开展了GDGTs分析测试研究,试图为其成因、来源、AOM作用、生源等提供信息。研究结果表明:SH7B站位96.5~225.2 m的岩心样品中,传统指标总有机碳的δ13C值和C/N值对南海神狐海域天然气水合物赋存段的沉积物之生源输入指示效果不明显;GDGTs主要以类异戊二烯GDGTs为主,水合物赋存段(155~177 m)较非水合物赋存段,支链GDGTs相对百分含量明显增多,类异戊二烯GDGTs相对百分含量明显减少。BIT值进一步明确说明:水合物赋存段比非水合物赋存段,沉积物的陆源有机质输入明显增多。前人研究表明~6 Ma左右南海北部接受了较强的河流碎屑和季风碎屑输入,此次事件造成水合物赋存段(6.0~6.74 Ma)陆源有机质输入增多,结果导致沉积物颗粒粒度增大,孔隙空间增多。较粗颗粒物的大量注入可以改善储层物性,形成上细下粗的有利储集体系,从而为神狐海域天然气水合物提供良好储集空间。
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出版历程
收稿日期:  2014-03-24
修回日期:  2014-05-18

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