鄂尔多斯盆地西缘奥陶系拉什仲组深水水道沉积类型及演化

李华; 何幼斌; 冯斌; 郝烃; 苏帅亦; 张灿; 王季欣

doi:10.3799/dqkx.2018.568

鄂尔多斯盆地西缘奥陶系拉什仲组深水水道沉积类型及演化

doi: 10.3799/dqkx.2018.568

李华^1,2,3,,
何幼斌^1,2,3, ,,
冯斌¹,
郝烃¹,
苏帅亦¹,
张灿¹,
王季欣¹

1.
长江大学地球科学学院, 湖北武汉 430100
2.
长江大学沉积盆地研究中心, 湖北武汉 430100
3.
长江大学油气资源与勘探技术教育部重点实验室, 湖北武汉 430100

基金项目:

国家自然基金项目 41472096

湖北省教育厅科学研究计划中青年人才项目 Q20171308

长江青年基金 2015cqn26

国家自然基金项目 41502101

湖北省创新群体基金 2015CFA024

详细信息

作者简介:
李华(1984-), 男, 讲师, 博士, 主要从事沉积学教学及科研

通讯作者:
何幼斌

中图分类号: P624
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- 被引次数: 0
出版历程
- 收稿日期: 2017-12-11
- 刊出日期: 2018-06-15

Type and Evolution of Deep-Water Channel Deposits of Ordovician Lashizhong Formation in Western Margin of Ordos Basin

Li Hua^{1,2,3
,},
He Youbin^{1,2,3
, ,},
Feng Bin¹,
Hao Ting¹,
Su Shuaiyi¹,
Zhang Can¹,
Wang Jixin¹

1.
School of Geosciences, Yangtze University, Wuhan 430100, China
2.
Research Center of Sedimentary Basin, Yangtze University, Wuhan 430100, China
3.
Key Laboratory of Exploration Technologies for Oil and Gas Resources, Ministry of Education, Yangtze University, Wuhan 430100, China

摘要

摘要: 深水水道沉积是深水区重要沉积类型之一，对其形成机制研究不仅能提高深水沉积认识，还能为油气勘探提供帮助.以露头资料为基础，对鄂尔多斯盆地西缘奥陶系拉什仲组深水水道形成机制进行了详细研究.拉什仲组岩性以灰绿色页岩及砂岩为主，另见少量的粉砂岩及砾岩.槽模、交错层理、粒序层理及变形构造等发育.总体反映深水沉积环境，重力流沉积较为发育.其中，深水水道沉积极为典型.根据形态、结构及沉积方式等，将研究区深水水道沉积划分为限制型和非限制型水道沉积.前者包括复合型及垂向加积型水道沉积，后者由迁移型及孤立型小水道沉积组成.复合型水道沉积厚约7.5 m，岩性以粗砂岩为主，底部见砾岩，水道轴部沉积、次级水道及水道-堤岸复合体沉积发育，可分为早期、中期和晚期.垂向加积型水道沉积宽为12.4 m，厚为1.3 m，宽深比为9.54，以中砂岩及细砂岩为主，水道内部以层状砂岩充填为主.迁移型水道沉积宽为6.9~12.3 m，厚为0.23~0.73 m，宽厚比14.11~53.48，以中-细砂岩为主，具有明显的北西向迁移特征；孤立型小水道沉积宽为0.5~0.6 m，厚为0.15~0.25 m，宽厚比为2.4~3.33，多为细砂-粉砂岩组成，透镜状，规模小.重力流爆发初期，能量高，侵蚀作用强，发育复合型及垂向加积型水道沉积；重力流中-后期，能量逐渐降低，迁移型水道沉积开始发育；在重力流后期及末期，其能量进一步降低，发育孤立型小水道沉积.而在空间位置上，复合型及垂向加积型水道沉积多发育在斜坡中上部，中部及下部发育迁移型水沉积道，斜坡脚及深海盆地以孤立型小水道沉积最为发育.
- 水道 /
- 浊流 /
- 拉什仲组 /
- 奥陶系 /
- 鄂尔多斯盆地 /
- 石油地质
Abstract: The deep-water channel sedimentary type is one of important sedimentary types in the deep-water zone. Research on the mechanism of deep-water channel not only can improve acquaintance of deep-water deposits, but also is helpful to oil and gas exploration. Mechanism of the deep-water channel of the Ordovician Lashizhong Formation in western margin of the Ordos basin was detailedly worked based on outcrop. The lithology of Lashizhong Formation consists of greyish-green mudstone and sandstone and few siltstone and conglomeration with flute cast, cross bedding, graded bedding and deformation structure, which suggests deep-water environment. Gravity flow deposits are well developed. The deep-water channel deposits are also typical. It is found in this study that the deep-water channel deposits could be divided into confined and non-confined channels, based on the morphology, structure, and sedimentary style. The former includes complex and vertical aggradation channel deposits. The latter can be subdivided into migrational channel and isolated small channel deposits. The lithology of complex channel deposits is coarse sandstone and conglomeration in the bottom, containing channel axis deposit, secondary channel and channel-levee system deposits, with 7.5 m in width, which could be divided into developmental, mature and decline phases. The vertical aggradation channel deposits are bedded medium and fine sandstone, with 12.4 m in width, 1.3 m in thickness, and the width-to-thickness ratio of 9.54. The migrational channel is medium to fine sandstone with northwestward migration. The width is 6.9-12.3 m, the thickness is 0.23-0.73 m, and width-to-thickness ratios range from 14.11-53.48. The isolated small channel deposits consist of fine sandstone and siltstone, lenticular shaped, small scale with 0.5-0.6 m in width, 0.15-0.25 m in thickness, and the width-to-thickness ratios of 2.4-3.33. The complex and vertical aggradation channel deposits develop when gravity flow outbreaks. Its energy is usually high with strong erosive power. The migrational channel deposits develop when gravity flow is in middle to later phases when their energy is damped. And the isolated small channel deposits develop during last phase of gravity flow. Its energy further decreases. In the spatial position, the complex and vertical channel deposits usually develop in the middle-upper part of slope. Migrational channel deposits form in the middle-lower slope, and isolated small channel deposits commonly grow in toe of slope and deep-water basin.
- channel /
- turbidity current /
- Lashizhong Formation /
- Ordovician /
- Ordos basin /
- petroleum geology

HTML全文

图 1 研究区位置及岩性特征

a和b为研究区位置及环境(据孙宜朴等，2008)；c为拉什仲组沉积特征(据肖彬等, 2014, 有修改)

Fig. 1. The location and lithology of the study area

下载: 全尺寸图片幻灯片

图 2 复合型水道沉积特征

a.水道野外照片宏观特征；b，c.水道内部充填特征，共13条次级水道；d~h.次级水道特征；g.为水道5侧翼，细砂－粉砂岩，交错层理发育；i.灰绿色泥岩夹薄层砂岩及粉砂岩

Fig. 2. Sedimentary characteristics of complex channels

下载: 全尺寸图片幻灯片

图 3 垂向加积型水道特征

a，b.砾岩，水道轴部沉积，含生屑；c，d.垂向加积水道，内部为砂岩充填

Fig. 3. Characteristics of vertical aggradation channels

下载: 全尺寸图片幻灯片

图 4 迁移型水道特征

a~c.迁移型水道，拉什仲组第一段，北西向迁移特征；a肖彬等(2014)；d.迁移型水道，拉什仲组第三段，水道具北西向迁移特征；e.爱尔兰北部石炭系Ross组迁移水道，侧积体发育

Fig. 4. Characteristics of migrational channels

下载: 全尺寸图片幻灯片

图 5 孤立型小水道沉积特征

“U”型，透镜状

Fig. 5. Sedimentary characteristics of isolated small channels

下载: 全尺寸图片幻灯片

图 6 研究区水道沉积模式

Fig. 6. The sedimentary model of deep-water channel deposits in the study area

下载: 全尺寸图片幻灯片

表 1 研究区水道沉积特征

Table 1. Sedimentary characteristics of channels in the study area

类型		沉积单元	规模	形状	岩性	沉积构造	沉积序列	重力流类型	沉积过程
限制型水道沉积	复合型水道沉积	轴部沉积、水道、溢流/堤岸	大	透镜状，“U”形、“V”形、复合形	砂岩为主，少量砾岩	槽模、平行层理、粒序层理、交错层理	下粗上细	碎屑流、浊流	侵蚀、过路、沉积
限制型水道沉积	垂向加积型水道沉积	轴部沉积、水道	较大	“U”形、“V”形	砂岩为主，少量粉砂岩	侵蚀面、平行层理、粒序层理	下粗上细	浊流	过路、沉积
非限制型水道沉积	迁移型水道沉积	水道、侧积体、溢流/堤岸	大	“U”形	砂岩	粒序层理、平行层理	下粗上细	浊流	过路、沉积
非限制型水道沉积	孤立型小水道沉积	水道、溢流/堤岸	小	“U”形	砂岩，粉砂岩	平行层理，变形构造	下粗上细	浊流	沉积

下载: 导出CSV

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