鄂尔多斯盆地奥陶系乌拉力克组沉积特征及其控源作用

席胜利; 李文厚; 黄正良; 刘燕

doi:10.16152/j.cnki.xdxbzr.2024-06-007

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鄂尔多斯盆地奥陶系乌拉力克组沉积特征及其控源作用

鄂尔多斯盆地岩相古地理与沉积演化 | 更新时间：2024-12-16

- 鄂尔多斯盆地奥陶系乌拉力克组沉积特征及其控源作用
- Sedimentary characteristics and controlling effect on source rocks in Wulalike Formation of Ordovician in Ordos Basin
- 西北大学学报（自然科学版） 2024年54卷第6期页码：1013-1022
- 作者机构：
  
  1.低渗透油气田勘探开发国家工程实验室/中国石油长庆油田公司，陕西　西安　 710018
  2.西北大学　地质学系，陕西　西安　 710069
  3.中国石油东方地球物理公司研究院长庆分院，陕西　西安　 710021
- 作者简介：
  
  席胜利，男，博士，正高级工程师，从事石油与天然气地质技术管理与研究，xsl_cq@petrochina.com.cn。
  黄正良，男，高级工程师，从事页岩气及海相碳酸盐岩勘探研究，hzl0915_cq@petrochina.com.cn
- 基金信息：
  
  中国石油天然气股份有限公司“十四五”前瞻性基础性重大科技项目(2021DJ1904);中国石油股份公司科技专项(2023ZZ16YJ01)
- DOI：10.16152/j.cnki.xdxbzr.2024-06-007
  中图分类号： TE122.3
- 纸质出版日期：2024-12-25，
  
  收稿日期：2024-09-15，
- 稿件说明：
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席胜利, 李文厚, 黄正良, 等. 鄂尔多斯盆地奥陶系乌拉力克组沉积特征及其控源作用[J]. 西北大学学报（自然科学版）, 2024,54(6):1013-1022.

XI SHENGLI, LI WENHOU, HUANG ZHENGLIANG, et al. Sedimentary characteristics and controlling effect on source rocks in Wulalike Formation of Ordovician in Ordos Basin. [J]. Journal of northwest university (natural science edition), 2024, 54(6): 1013-1022.
席胜利, 李文厚, 黄正良, 等. 鄂尔多斯盆地奥陶系乌拉力克组沉积特征及其控源作用[J]. 西北大学学报（自然科学版）, 2024,54(6):1013-1022. DOI： 10.16152/j.cnki.xdxbzr.2024-06-007.

XI SHENGLI, LI WENHOU, HUANG ZHENGLIANG, et al. Sedimentary characteristics and controlling effect on source rocks in Wulalike Formation of Ordovician in Ordos Basin. [J]. Journal of northwest university (natural science edition), 2024, 54(6): 1013-1022. DOI： 10.16152/j.cnki.xdxbzr.2024-06-007.

摘要

鄂尔多斯盆地奥陶系上统乌拉力克组发育一套分布稳定的黑色页岩，为盆地奥陶系的优质烃源岩层，近期多口探井获得工业油气流，证实了具有较好的勘探潜力。勘探研究证实，优质烃源岩分布为页岩气富集的基础，因此，系统开展乌拉力克期沉积特征及对优质烃源岩的控制作用研究，对于寻找优质页岩及指导下一步勘探方向意义重大。通过系统开展沉积特征及地球化学特征研究，建立了乌拉力克期沉积模式，明确了优质烃源岩分布规律。①乌拉力克组平面上稳定分布，整体具有“西厚东薄”的特征，主要发育盆地相、广海陆棚相、斜坡相三类大相，斜坡相可细分为上斜坡亚相和下斜坡亚相两类亚相。②建立了乌拉力克期沉积模式：盆地西部乌拉力克期属祁连海域，为台地边缘型沉积，水体整体具有“西深东浅，南深北浅”的沉积格局，斜坡坡度较大，相变快。③乌拉力克组发育一套低有机质丰度页岩，有机质含量的变化主要受页岩纹层矿物成分、沉积相带、沉积层序控制。结论认为，鄂尔多斯盆地西部地区乌拉力克期发育一套台地边缘沉积，广海陆棚相、下斜坡亚相黑色页岩发育，有机质丰度高，为有利相带，优质页岩主要分布在底部20～30 m范围内。

Abstract

It developes thick shale with stable distribution and it is the best source rock in Wulalike Formation of Ordovician in Ordos Basin. Many exploration wells have obtained high production of industrial oil and gas recently

it shows a good exploration situation. It has significance to study sedimentary characteristics and controlling effect on high-quality source rocks’distribution. Based on the study of sedimentary characteristics and geochemical characteristics

it shows that: ① Wulalike Formation distribute extensively and characterd by ”thick in the west and thin in the east”

it developes basin facies

open shelf facies and slope facies

slope facies includes upper slope subfacies and lower slope subfacies. ②It belongs to the Qilian Sea in Wulalike period

seawater is deep in the west and shallow in the east

deep in the south and shallow in the north

the slope grade is large and the facies transition is fast. ③It developes low-abundance shales in the Wulalike Formation and the spatial distribution of high-quality shales is mainly controlled by the mineral composition

sedimentary facies and sedimentary sequence. The conclusion is that open shelf facies and lower slope subfacies are favorable facies

high-quality shales are mainly distributed in the bottom 20～30 m range.

关键词

鄂尔多斯盆地西部乌拉力克组广海陆棚相下斜坡亚相优质烃源岩

Keywords

western Ordos BasinWulalike Formationopen shelf facieslower slope subfacieshigh-quality source rocks

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