珠江口盆地白云深水区珠海组石英颗粒表面特征

doi:10.11885/j.issn.1674-5086.2015.09.04.03

西南石油大学学报(自然科学版) ›› 2017, Vol. 39 ›› Issue (1): 1-11.DOI: 10.11885/j.issn.1674-5086.2015.09.04.03

• 地质勘探 • 下一篇

珠江口盆地白云深水区珠海组石英颗粒表面特征

邢作昌¹, 林畅松², 秦成岗³, 张忠涛³, 王思琦¹

1. 中国地质大学(北京)能源学院, 北京海淀 100083;
2. 中国地质大学(北京)海洋学院, 北京海淀 100083;
3. 中海石油(中国)有限公司深圳分公司研究院, 广东广州 510240

收稿日期:2015-09-04 出版日期:2017-02-01 发布日期:2017-02-01
通讯作者: 林畅松,E-mail:Lincs@cugb.edu.cn
作者简介:邢作昌,1988年生,男,汉族,河南新乡人,博士研究生,主要从事层序沉积地质研究。E-mail:xzcxing@163.com;林畅松,1958年生,男,汉族,广东遂溪人,教授,博士生导师,主要从事沉积地质和含能源沉积盆地的研究和教学工作。E-mail:Lincs@cugb.edu.cn;秦成岗,1974年生,男,汉族,山西沁县人,高级工程师,主要从事石油地质与油气勘探研究工作。E-mail:qinchg@cnooc.com.cn;张忠涛,1977年生,男,汉族,辽宁西丰人,高级工程师,主要从事含油气盆地地质综合研究与勘探目标评价工作。E-mail:zhangzht@cnooc.com.cn;王思琦,1992年生,女,汉族,黑龙江大庆人,硕士,主要从事沉积学和层序地层学方面的研究。Email:1442666216@qq.com
基金资助:
国家自然科学基金重点项目（91328201）。

The Surface Features of the Quartz Sand Grains in Zhuhai Formation of Baiyun Deep-water Area, the Pearl River Mouth Basin

XING Zuochang¹, LIN Changsong², QIN Chenggang³, ZHANG Zhongtao³, WANG Siqi¹

1. School of Energy Resources, China University of Geosciences(Beijing), Haidian, Beijing 100083, China;
2. School of Ocean Sciences, China University of Geosciences(Beijing), Haidian, Beijing 100083, China;
3. Research Institute of Shenzhen Branch, CNOOC, Guangzhou, Guangdong 510240, China

Received:2015-09-04 Online:2017-02-01 Published:2017-02-01

摘要/Abstract

摘要： 石英具有较大的硬度和较高的化学稳定性，较好地保留了搬运和沉积过程中各种地质营力所形成的微观形貌特征，这些微观形貌可为沉积物搬运机制、沉积环境解释提供依据。通过对珠江口盆地白云凹陷深水区珠海组单颗粒石英的表面形貌特征的研究发现，该组的沉积石英颗粒表面微观形貌类型可划分为机械、化学、机械-化学成因等3大类和26小类。其中以次棱角状、V形撞击坑、直弯沟/刻痕、机械上翻片、磨蚀疲劳等碰撞磨蚀压刻等机械成因的微观形貌特征最为突出，表明研究区珠海晚期的沉积作用以中等的搬运距离、高能的水动力条件（上部流动体制）和跃移为主的搬运机制为特征。该研究填补了中国深水区此项研究的空白，虽然这些微观形貌的具体沉积环境意义还有待深入研究，但这将为沉积过程的研究提供新的思路和证据。

关键词: 白云深水区, 珠海组, 单颗粒石英, 微观结构, 扫描电镜

Abstract: Due to the hardness and chemical stability of quartz grains, their surfaces contain numerous microtextures that are formed during transport and deposition by various geological forces. These microtextures can provide evidence for interpreting sedimentary environments and transport mechanisms. The causes of sedimentary quartz grain surface microtextures in the Zhuhai Formation, Baiyun deep-water area, can be divided into three categories, mechanical, chemical, and mechanicalchemical, with 26 subclasses. The most dominant characteristics are subangular shape, V-shaped percussion cracks, straight/curved grooves and scratches, upturned plates, and abrasion fatigue. Sedimentary deposition in the late-Zhuhai Formation in the study area is characterized by medium transport distance, high-energy hydrodynamics(upper flow regime), and saltation. Although the specific sedimentary environment significance of the microfeatures remains to be addressed, this study provides new ideas and evidence for understanding sedimentary processes.

Key words: Baiyun deep-water area, Zhuhai Formation, single quartz grain, microtexture, SEM

中图分类号:

TE135

邢作昌, 林畅松, 秦成岗, 张忠涛, 王思琦. 珠江口盆地白云深水区珠海组石英颗粒表面特征[J]. 西南石油大学学报(自然科学版), 2017, 39(1): 1-11.

XING Zuochang, LIN Changsong, QIN Chenggang, ZHANG Zhongtao, WANG Siqi. The Surface Features of the Quartz Sand Grains in Zhuhai Formation of Baiyun Deep-water Area, the Pearl River Mouth Basin[J]. 西南石油大学学报(自然科学版), 2017, 39(1): 1-11.

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珠江口盆地白云深水区珠海组石英颗粒表面特征

The Surface Features of the Quartz Sand Grains in Zhuhai Formation of Baiyun Deep-water Area, the Pearl River Mouth Basin

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