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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第41卷

期数:

2019年第04期

页码:

491-504

栏目:

基础地质与矿产地质

出版日期:

2019-07-15

文章信息/Info

Title:

Finely Outcrop Analysis of Deep Water Sandstones from Yanchang Formation in Zichang Area of Ordos Basin, China

文章编号:

1672-6561(2019)04-0491-14

作者:

江涧¹; 2; 3; 赵俊峰¹; 2*; 李嫄¹; 4

(1. 西北大学 地质学系,陕西 西安 710069; 2. 西北大学 大陆动力学国家重点实验室,陕西 西安 710069; 3. 合肥工业大学 资源与环境工程学院,安徽 合肥 230009; 4. 中国石油长庆油田分公司第一采气厂,陕西 靖边 718500)

Author(s):

JIANG Jian¹; 2; 3;  ZHAO Jun-feng¹; 2*;  LI Yuan¹; 4

(1. Department of Geology, Northwest University, Xi’an 710069, Shaanxi, China; 2. State Key Laboratory of Continental Dynamics, Northwest University, Xi’an 710069, Shaanxi, China; 3. School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, Anhui, China; 4. No.1 Natural Gas Plant, Changqing Oilfield Company, PetroChina, Jingbian 718500, Shaanxi, China)

关键词:

深水沉积;  浊积砂岩;  露头;  岩相;  等级界面;  构型单元;  延长组;  鄂尔多斯盆地

Keywords:

deep-water deposition;  turbidite sandstone;  outcrop;  lithofacies;  bounding surface hierarchy;  architectural element;  Yanchang Formation;  Ordos Basin

分类号:

P586

DOI:

-

文献标志码:

A

摘要:

鄂尔多斯盆地子长地区广泛出露延长组长1油层组深湖相浊积砂岩,在露头观测的基础上对其进行了构型单元分析。研究区长1油层组内可见7种岩相类型,分别为块状砂岩相(Sm)、具撕裂屑块状砂岩相(Smt)、平行层理砂岩相(Sh)、沙纹交错层理粉砂岩相(Fr)、同生变形构造粉砂岩相(Fd)、水平层理粉砂岩相(Fl)与块状泥岩相(Fm); 识别出水道(CH)、堤岸(LV)和朵体(LB)3种不同类型的构型单元。根据水道构型单元垂向上的岩相组合和空间分布特点,将水道分为4类,对应于浊积扇体的不同部位:在上扇区域,主要发育Ⅰ类水道(Smt-Fm-Sm),砂体横向延伸有限; 在中扇区域,主要发育Ⅱ类水道(Sm-Sh-Fr-Fl-Fm)与Ⅲ类水道(Sm-Fr-Fl-Fm),这两类砂体延伸性较好,是子长地区长1油层组深水砂体的主要组成部分; 在下扇区域,发育Ⅳ类水道(Sm-Fl-Fm)。根据水道类型的差别探索提出子长地区长1油层组深水砂体沉积模式。

Abstract:

The deep lacustrine turbidite sandstone widely develops in Chang-1 interval of Triassic Yanchang Formation, and well exposes in Zichang area of the central Ordos Basin. Based on outcrop observation, the deep lacustrine turbidite sandstone was finely analyzed to study the sedimentary architectural elements of the lacustrine turbidite sandstone. 7 different types of lithofacies, including massive sandstone facies(Sm), massive sandstone facies with teared intraclasts(Smt), parallel bedding sandstone facies(Sh), ripple cross bedding siltstone facies(Fr), contemporaneous deformed structural siltstone facies(Fd), horizontal lamination siltstone facies(Fl)and mudstone facies(Fm), were summarized in Chang-1 interval of Zichang area; and 3 kinds of architectural elements, including channel(CH), levee(LV)and lobe(LB), were recognized. The channel architectural elements can be further divided into 4 types according to their vertical association of lithofacies and spatial distribution characteristics, which correspond to different parts of turbidite fan. In the upper fan area, channel Ⅰ(Smt-Fm-Sm)is developed, and the lateral extensibility of sand body is limited. The middle fan area is mainly composed of channel Ⅱ(Sm-Sh-Fr-Fl-Fm)and channel Ⅲ(Sm-Fr-Fl-Fm); the two types of sandbodies have very large extensibility and are the main components of deep-water sandbodies of Chang-1 interval in Zichang area. In the lower fan area, channel Ⅳ(Sm-Fl-Fm)with poor lateral extensibility is developed. According to the distinction of different types of channels, the depositional model for deep water sandstones of Chang-1 interval in Zichang area was preliminarily proposed.

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　FENG Bin,LI Hua,HE You-bin,et al.Characteristics of Milankovitch Cycles in Deep Water Contourites—A Case Study of Upper Ordovician Zhaolaoyu Formation in Fuping Area of Shaanxi, China[J].Journal of Earth Sciences and Environment,2019,41(04):69.
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备注/Memo

备注/Memo:

收稿日期:2019-04-13; 修回日期:2019-05-20投稿网址:http://jese.chd.edu.cn/
基金项目:国家基础科学人才培养基金地质学科学研究培训项目(XDCX2015-18); 国家重点研发计划项目(2017YFC0603106)
作者简介:江涧(1995-),男,江西上饶人,合肥工业大学理学硕士研究生,E-mail:2734365251@qq.com。
*通讯作者:赵俊峰(1975-),男,山西晋中人,副教授,博士研究生导师,工学博士,E-mail:zjf@nwu.edu.cn。

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更新日期/Last Update: 2019-07-11