塔里木盆地塔中—顺托果勒地区奥陶系良里塔格组碳酸盐岩颗粒滩沉积特征

doi:10.13278/j.cnki.jjuese.20170307

吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (3): 621-636.doi: 10.13278/j.cnki.jjuese.20170307

• 地质与资源 • 下一篇

塔里木盆地塔中—顺托果勒地区奥陶系良里塔格组碳酸盐岩颗粒滩沉积特征

鄢伟^1,2,3, 张光学^1,2,3, 樊太亮⁴, 夏斌¹, 高志前⁴, 张莉^2,3, 杨振^2,3, 强坤生^2,3

1. 中山大学海洋学院, 广州 510075;
2. 广州海洋地质调查局海底矿产资源重点实验室, 广州 510760;
3. 广州海洋地质调查局海洋石油天然气地质研究中心, 广州 510760;
4. 中国地质大学(北京)能源学院, 北京 100083

收稿日期:2017-11-24 出版日期:2019-06-03 发布日期:2019-06-03
作者简介:鄢伟(1987-),男,在站博士后,主要从事碳酸盐岩沉积和储层方面的研究,E-mail:yanwei021066@126.com
基金资助:
自然资源部海底矿产资源重点实验室开放基金（KLMMR-2017-A-16）；中国地质调查局项目（DD20191009，DD20160155）

Sedimentary Characteristics of Carbonate Shoals of Ordovician Lianglitage Formation in Tazhong and Shuntuoguole Area, Tarim Basin

Yan Wei^1,2,3, Zhang Guangxue^1,2,3, Fan Tailiang⁴, Xia Bin¹, Gao Zhiqian⁴, Zhang Li^2,3, Yang Zhen^2,3, Qiang Kunsheng^2,3

1. Marine Institute, Sun Yat-Sen University, Guangzhou 510075, China;
2. Key Laboratory of Marine Mineral Resources, Guangzhou Marine Geological Survey, Guangzhou 510760, China;
3. Marine Petroleum and Gas Geological Research Center, Guangzhou Marine Geological Survey, Guangzhou 510760, China;
4. School of Energy Resources, China University of Geosciences, Beijing 100083, China

Received:2017-11-24 Online:2019-06-03 Published:2019-06-03
Supported by:
Supported by Open Fund of MNR Key Laboratory of Marine Mineral Resources (KLMMR-2017-A-16) and Geolo-gical Investigation of China Geological Survey (DD20191009,DD20160155)

摘要/Abstract

摘要： 塔中-顺托果勒地区奥陶系颗粒滩具有良好的油气资源前景。本文介绍了碳酸盐岩颗粒滩的定义和研究概况。通过镜下薄片分析将该地区良里塔格组碳酸盐岩颗粒滩主要划分为3类，并明确了3类颗粒滩的微观沉积特征。颗粒滩主要类型为：内碎屑滩、生物碎屑滩和鲕粒滩，所含的主要颗粒类型分别是内碎屑（砂屑为主，含砾屑）、生物碎屑和鲕粒，多为亮晶胶结，反映了高能水动力环境，由于迁移作用颗粒时常会相互伴生。另外，也发现了在低能环境中发育的复鲕和中-高能水动力环境下的藻粒；藻粒常常会与内碎屑颗粒、生物碎屑颗粒伴生，规模不大，多形成于中-高能水动力环境下的碳酸盐岩潮坪环境或台缘缓坡带。通过连井对比分析可以得出，良里塔格组可以划分为3个三级层序，海侵体系域主要以薄层退积为主，高位体系域以厚层加积为主。最后，本文结合颗粒滩的展布特征建立了该地区良里塔格组颗粒滩沉积模式。

关键词: 塔里木盆地, 奥陶系, 碳酸盐岩颗粒滩, 沉积特征, 沉积模式, 良里塔格组

Abstract: The Ordovician carbonate shoals in Tazhong and Shuntuoguole area have good prospects for hydrocarbon resources. The definition and classification of carbonate shoals are clarified in this paper. Based on the analysis of thin sections, the carbonate shoals of Lianglitage Formation could be classified into three types:intra-clastic shoal, oolitic shoal and bioclastic shoal, containing mainly intra-clast, bio-clast, and ooid. Most of the carbonate shoals are bright crystal cement, reflecting a high-energy hydrodynamic environment. Different grains are often associated with each other because of migration. The compound ooid developed in low energy environment and the algae grain from middle-high energy environment are also identified. Algae grains are developed usually together with intra-clast and bio-clast, although not abundant, and formed in a middle-high energy tidal flat environment and gentle slope of carbonate platform. The cementation type, separation and grinding are affected by the energy of sedimentary environment and hydrodynamic conditions. Through the comparison analysis of connecting wells, Lianglitage Formation could be subdivided into three third-order sequences. The stacking pattern of carbonate shoals in transgressive system tract is thin-layer cake retrograde deposit, while in high system tract that is thick-layer cake deposit. At last, the sedimentary model of carbonate shoals in this area is built through combining their distribution characteristics.

Key words: Tarim basin, Ordovician, carbonate shoals, sedimentary characteristics, sedimentary model, Lianglitage Formation

中图分类号:

TE122

鄢伟, 张光学, 樊太亮, 夏斌, 高志前, 张莉, 杨振, 强坤生. 塔里木盆地塔中—顺托果勒地区奥陶系良里塔格组碳酸盐岩颗粒滩沉积特征[J]. 吉林大学学报(地球科学版), 2019, 49(3): 621-636.

Yan Wei, Zhang Guangxue, Fan Tailiang, Xia Bin, Gao Zhiqian, Zhang Li, Yang Zhen, Qiang Kunsheng. Sedimentary Characteristics of Carbonate Shoals of Ordovician Lianglitage Formation in Tazhong and Shuntuoguole Area, Tarim Basin[J]. Journal of Jilin University(Earth Science Edition), 2019, 49(3): 621-636.

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塔里木盆地塔中—顺托果勒地区奥陶系良里塔格组碳酸盐岩颗粒滩沉积特征

Sedimentary Characteristics of Carbonate Shoals of Ordovician Lianglitage Formation in Tazhong and Shuntuoguole Area, Tarim Basin

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